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The Earth Observatory of Singapore

The Earth Observatory of Singapore

EOSThe Earth Observatory of Singapore

1 The Year at EOS

Director’s Welcome · · · 3

Featured Projects · Ancient Tsunami Records · 4 · Surface Rupture Found · 6 · Explosivity of Merapi · 8 · Typhoon Haiyan · 10 · The EOS ART Projects · 12

Research · Climate · · · · · 16 · · Tectonics · · · 20 · · · Volcano · · · 25 · · · · Art+Media · 28

Monitoring Hazards · · · · 30 Sustainability · · · · 32 Education and Outreach · · · 33 Degree Programs · · · · 34 Research Documents · · · · 36 Research Technology · · · · 44 Research Map · · · · 46 Prime Minister Lee Visit · · · · 48 Financial Statements and Staffing · · 50 Credits · · · · · 52

2 1 Earth Observatory of Singapore Director’s Message

The fundamental goal of the Earth Observatory is to understand how our works, and use that knowledge to help individuals and societies live and prosper in a sustainable way. This is in line with Singapore’s four principal goals for its program of Research Centres of Excellence, begun over seven years ago. Looking over our accomplishments in this year’s annual report I am pleased to see that the country’s first big effort in the Earth Sciences is Prof. Kerry Sieh achieving these objectives. Director We continue to attract and support top-quality researchers from Singapore and all over the globe. We have been able to build a scientific infrastructure, ranging from geochemical laboratories and computational facilities here on campus to geophysical networks with our colleagues in neighboring countries. We have become a regional and global nexus for geohazards research in Southeast Asia, and we seek to be an enduring magnet for retention of research talent for decades to come. We are accomplishing excellent and impactful research with global impact and relevance to Singapore. The past year saw the publication of papers that will have important impacts in our research arenas. Alongside with our curiosity-driven research, our Applied Projects Group, formerly the Sustainability Group, is moving closer to meeting the immediate research needs of regional governments, businesses and communities. We made great progress this past year in meeting our mandate to nurture Singapore’s own young talent. Throughout 2013, EOS staff took the lead in conceiving of NTU’s new Asian School of the Environment. We now offer a new major in Environmental Earth Systems Science and a minor in Environmental Sustainability. We have developed strong research collaborations in the region and abroad. Just as important, we are raising the awareness of geohazards in our classrooms and in the regional public arena. Young woman work- ing in the fields near And we are building durable bridges with our Southeast Asian Bardibas, Nepal. neighbors through research, training, and collaboration.

2 3 Earth Observatory of Singapore Ancient Tsunami Records Charles Rubin, Kerry Sieh and Patrick Daly

EOS scientists are actively exploring for new records of ancient tsunami events in Aceh Province, Indonesia. The team recently discovered a cave near the beach that is protected from the waves and stands over a meter above the tide. Digging into the cavern floor, the scientists discovered perfectly preserved layers of sandy sediments left behind from tsunamis over the past 8000 years. The discovery of such well-preserved tsunami records has the potential to increase our understanding of Above: Charles Rubin (R) natural hazards in West Sumatra. and Kerry Sieh (L) examine sediment deposits under Radiocarbon analysis of charcoal the glow of fluorescent fragments and shells suggest the interval lights. between tsunamis is on average every 400 years. But variable recurrence intervals hint that events may occur in flurries of closely-timed ruptures.. Thus far, evidence of tsunami events has been found, including the devastating 2004 Indian Ocean tsunami event that claimed the lives of nearly 250,000 people. The EOS team is in the process of using EOS scientists discovered Kerry Sieh explains the this data to fine-tune the timeline of a hidden cave close to a different rock layers that beach in Aceh Province. have been deposited over earthquakes and tsunamis in the region. several millenia. However, this evidence is still insufficient Above: Beautiful trench Top left: The scientists Top of page: Charles Rubin to predict with absolute certainty when the wall reveals tsunami discuss the relations (L) and Kerry Sieh (R) take next tsunami will take place. The insights events and fracturing from between layers of tsu- measurements along the gained from this discovery will help ground shaking. The 2004 nami sand and organic bat coastline south of Banda tsunami sand sits atop guano. Counterclockwise, Aceh. communities along Aceh’s coast to better multiple ancient tsunamis. L to R: Kerry Sieh, Charles prepare for such disasters. Rubin, Patrick Daly, Jedrzej Majewski, and Ben Hor- ton.

4 5 Tsunami Stratigraphy Tsunami Stratigraphy Nepal Surface Rupture Paul Tapponnier

The last earthquake to occur in the Himalayas was the MW~8.2 Bihar-Nepal earthquake in 1934, one of the most devastating quakes Nepal and India had experienced. Paul Tapponnier’s team ruled out an 80-year-old consensus when they found a surface rupture at the thrust’s fault and proved that the latest great Himalayan faults were not “blind.” Paul Tapponnier searches Top of page: An aerial Map: The team mapped Opposite page, top: The for charcoal samples to be view of the Himalayan the active faults and amount and size of char- With a preliminary record of seven great earthquakes in the last used in radiocarbon dating. Front with the Sir Khola geomorphology of the Sir coal specimen given to the 4,500 years, the team found out that two had ruptured the surface. Charcoal is sampled where and Jangha rivers cutting Khola outlet on a high-res- processing laboratory is Through morphological and paleoseismological studies along active faults occur. across the vast Gangetic olution topographic image. crucial in ensuring accurate plain. Photographing rep- Map from et al., radiocarbon dating. the active Main Frontal Thrust, they uncovered traces of the 1934 Research fellows extract- resents a powerful way to 2013. quake’s surface rupture in the Sir Khola and adjacent valleys. They ing charcoal specimens in a 1.5-meter trench. gather evidence that can also discovered that the AD 1255 earthquake that had devastated be used to find indicators RESEARCH # of active faulting. Kathmandu also broke the surface at the same place, providing the 73 first return time of 680 years of such catastrophic earthquakes.

6 7 Tectonics Tectonics Explosivity of Merapi Fidel Costa

Merapi is one of the most explosive volcanoes in Southeast Asia and the world. In 2010 the volcano produced its largest and most explosive eruption in over a century. Even as it remains one of the most hazardous volcanoes in the world, little is known about Merapi and the processes that control the timing and size of its eruptions. Fidel Costa and his team have embarked on a study of the explosive eruptions of Merapi, hoping to unravel these processes with the early monitoring signals before the eruption. Through geochemical and mineralogical studies, Fidel Costa’s team was able to determine that the cause of the eruption was the fast ascent of a voluminous, bubble-rich, Mg hot liquid from over 30 kilometers under the volcano. The clues to what could have triggered the eruption are locked in the structure of the crystals found in volcanic rocks. The patterns of elements found in these crystals are

Mount Merapi spews Fidel Costa (second from good indicators of the volcanic processes sulphuric gases due to left) explains volcanic phe- because crystals are shaped by changes in seismic activity. This type nomena during the teach- gas composition and temperature, similar of event might take place ers’ field seminar at Mount for weeks at a time. Merapi, Indonesia. to how tree rings record changes in climate and environment. Al K

Top of page: View of The research conducted the cause of explosive Merapi on a windy day by the forensic Volcano eruptions. Viewed through just before it is hidden by Petrology team involves an electron microscope clouds. analysing Merapi’s volcanic this amphibole crystal rocks. This aids in under- shows areas with varying standing the processes concentrations of mag- that take place inside nesium (top, yellow), RESEARCH # magma chambers during aluminum (green) and 14 eruptions. The team is one potassium (blue). step closer to unraveling

8 9 Volcanic Petrology Volcanic Petrology Typhoon Haiyan Adam Switzer

In November 2013, super typhoon Haiyan struck central Philippines, leaving a trail of damage in its wake. The Coastal Lab team, headed by Adam Switzer, conducted storm surge reconnaissance in the vicinity of San Pedro Bay and in the coastal city of Tacloban–the worst-hit city in the country. They also interviewed eyewitnesses and analyzed video recordings. The scientists also paired their surveys with other analyses in order to characterize Super typhoon Haiyan’s inundation. Using digitized local bathymetric charts and Delft3D Flow software, they generated a model that simulated surge heights on the open coast and within San Pedro Bay and compared it with a 1897 typhoon— Top of page: Survivors Ships washed ashore by dubbed Ty 1897 by EOS scientists— of recount their personal the 7 meter storm surge in similar magnitude. Storm surge heights experience of the storm Anibong village, just north from Ty 1897 ranged from four to seven surge while PhD student of downtown Tacloban. Lea Acierto Soria listens. Two months after the meters, devastating cities as it crossed the The accounts of the event, stilt houses were Philippines in a similar path. The team found survivors on the timing rebuilt seaward of the out that Haiyan, with surge heights of five and depth of flooding are stranded ships. valuable in reconstructing Scientists take auger Scientists measure to seven meters, was unprecedented in and validating storm surge cores to discover the thick- maximum flood heights San Pedro Bay but comparable to Ty 1897 models. Tacloban City, ness and extent of the in Tacloban City based on on the open Pacific coast. Together with its Leyte November 2013. sand eroded mostly from survivors accounts. Coast- the beach and deposited al lab scientists investigate 1897 predecessor, Haiyan teaches lessons Scientists measure reef inland by the storm surge the geological record of on disaster awareness, response, and boulders transported in Tanauan, Leyte. storms and tsunamis in mitigation; all issues relevant to sustainable during typhoon Haiyan Southeast Asia. societies. on a wave-cut terrace in Hernani, Samar.

RESEARCH # 82–96–97

10 11 Coastal Hazards Coastal Hazards The Possibility of Knowing, by Robert Zhao Renhui, is The EOS ART Projects part of a project of images about the Indonesian cit- ies of Padang and Banda Clara Balaguer, Carlos Casas, Chen Sai Hua Kuan, Aceh. Isaac Kerlow, Sutthirat Supaparinya, Robert Zhao, and Zhang Xiao

Above: Coastline, by Zhang Xiao presents hu- man life along the Chinese coast as well as some of its negative impact on the natural environment. This image presents a group Opposite page, lower Above (L and R): Lupang is a project about the of construction workers right: Sound of the Earth, by Clara Balaguer and uneasy relation between in Shandong coming into by Chen Sai Hua Kuan is Carlos Casas. These stills Man and Nature. Multi- contact with the sea for an experimental sound of the video installation lingual signs in English, the first time. installation that harnesses feature a member of the Chinese, Malay, and Tamil the power of wet soil to Ayta tribe relocated to a list some of the destruc- produce sound. new area after the Mount tive actions typical of Cover of the exhibition cat- The six projects produced between 2010 and Pinatubo eruption. natural hazards. alog featuring a still frame 2013 under the art residencies at EOS are from When Need Moves the Earth, by Sutthirat inspired by Earth science, natural hazards, Supaparinya is a video and humans living in high risk areas. installation of an explosion These interdisciplinary projects were of a coal mine reflects the possible consequences showcased at the Singapore Art Museum of human activities on the as part of the Unearthed exhibition, and environment. augmented with a series of seminars for young students about the interactions of science and art. RESEARCH # 34

12 13 Visiting Artists Visiting Artists Climate Research Indo-Pacific Hydroclimatic Variability 气候 Wang Xianfeng

Iklim

தட்ப வெப்பம் The tropical Indo-Pacific Oceans hold the warmest ocean water in the world, and are crucial to maintaining the balance between global atmospheric water and energy in this region. Any dramatic hydroclimatic change here may threaten the livelihood of more than half of the world’s population. Funded by a NRF fellowship and collaborating with colleagues from neighboring countries, the Isotope Geochemistry team is working to reconstruct the spatial and temporal pattern of rainfall change in the tropical Indo-Pacific by using cave carbonates called speleothems. High-precision uranium-thorium (U/Th) dating techniques are used to determine the ages of these speleothem samples. Stable isotope and trace metal analysis are also employed in the reconstruction of regional rainfall patterns. The knowledge acquired can be An EOS scientist reaches used to understand three issues: up to examine a speleo- them in a Myanmar cave. how astronomical forcing drives the Samples from these hydroclimate change in the Indo-Pacific; hidden carbonates can pro- whether the tropical Indo-Pacific was vide insight into historical rainfall patterns. dry during the glacial maximums; and if Climate research at EOS concentrates on regional the monsoonal rainfall in the region has climate monitoring, and the measurement and already been disrupted by the effects of modeling of past and modern tropical climates. human activities. EOS aims to fill a gap of much-needed information RESEARCH # on climatic forces in Southeast Asia, including the 11–12–19–22 Western Pacific Warm Pool and the Indian Ocean Dipole, which will allow better prediction of regional 77–88–90 consequences that can expected from global cli- mate change. 14 15 Isotope Geochemistry Haze from Forest Fires Unlocking Climate in Southeast Asia Secrets Nathalie Goodkin Mikinori Kuwata

Teamwork and coordina- tion is required when carrying out labor-intensive fieldwork. A hydraulic drill is used to extract coral samples off the coast of south Taiwan.

A peat swamp forest in Peat swamps are a big reservoir of carbon and they are abundant Sumatra is burned to clear in Kalimantan (Borneo) and Sumatra. Peat becomes the fuel that land for plantations. The atmospheric chemistry keeps the forest fires going—a peat layer can range from five to ten research team currently meters thick. focuses on investigating Maximally between 30 to 50 centimeters of peat up when the chemical composition and properties of aerosol a forest fire starts, which means that a lot of fuel is burnt within a particles emitted by tropi- small area. The amount of carbon accumulated in peat makes it cal Asia’s forest fires. Haze difficult to completely extinguish forest fires once they start. In 1997, from forest fires reduces visibility and poses a haz- for example, during one of the most heated forest fires in Indonesia, ard to air travel. the carbon fuel consumption of peat fire alone accounted for nearly The Marine Geochemistry team traveled to Checheng, Southern Nathalie Goodkin passes 40% of Indonesia’s fuel consumption that year. Taiwan, to investigate Earth’s climate history through the study of a sample of Porites coral to a scientist aboard the By tracing the chemistry of particles emitted from peat burning, corals. This region is where the Kuroshio Current intrudes into the research vessel. the team seeks to arrive at a more accurate simulation of haze in the South China Sea. They extracted samples of the Porites coral spe- Southeast Asia. cies that are approximately 300 to 500 years old, as well as seawa- ter in which these corals grow. Because the chemical composition of corals depend on the sea- water in which they grow, testing the coral samples can give an indication of the temperature and salinity of the surrounding seawa- ter. With these results, the team is able to reconstruct global climate and weather systems throughout several centuries. RESEARCH # RESEARCH # 40 4–64–94

16 17 Atmospheric Chemistry Marine Geochemistry Singapore’s Hydroclimate Weather and Climate Qin Xiaosheng Cycles in SE Asia Koh Tieh Yong

The Hydroclimatology group focuses on deriving statistical relationships and 0-3am forecasting smaller-scale weather details based on large-scale climate variables. The aim of the research is to develop tools and a framework to better understand local weather and climate. This project involves characterizing Singapore’s rainfall intensity distribution and its multiscale variability by using 12-3pm In the Southeast Asian region, rain statistics called L-moments to identify rain frequently occurs in a 24 hourly rates over a period of time. These ratios pattern. Koh Tieh Yong’s Tropical are then compared between probability Atmosphere team investigates this models (theoretical three-parameter skewed weather pattern, also called the distributions) to determine which best suits 3-6pm diurnal cycle. precipitation rates. During the day, the sun warms up

To understand temporal Besides investigating products that landmasses, and this rapid heating of and spatial structure of measure precipitation in Singapore, the the land destabilizes the atmosphere rainfall in Singapore and scientists also characterise and model the over the land. The temperature surrounding regions for 6-9pm a wide range of scales, small-scale spatial structure of local rainfall. in the atmosphere fluctuates, and to study their impact This is crucial to both the distribution of triggering a movement of fluids in on urban hydrology under rainfall data breakdown and its analysis the atmosphere that converts cloud changing climate condi- tions. from master to satellite stations. The water into rainfall over land in the findings yielded may facilitate other climate 9-12pm late afternoon. At night, with no solar change studies and the assessment of flood heat, the cooling effect at the top of risks in Singapore. the troposphere creates more cloud water, which in turn causes more These time simulations rainfall over open seas. created for the tropical at- mosphere research show 3-hour average accumulat- ed rain samples through- out the day, in Singapore RESEARCH # time (SGT). 31–50–51 RESEARCH # 52–55 39

18 19 Hydroclimatology Tropical Atmosphere Tectonics Research When the Earth Ticks Like a Clock Sylvain Barbot

RED LINES: PORE PRESSURE GREY LINES TREMOR HISTORY

Period of Pore Pressure Decrease TIME SINCE PREVIOUS EVENT (DAYS) TIME SINCE PREVIOUS EVENT CHANGE IN EFFECTIVE PORE PRESSURE (%)

Tektonik Period of Pore Pressure Increase EVENT DURATION IN SECONDS டெக்டானிக்ஸ் DIRECT EFFECT TIME (YEARS) 地质构造 Parkfield is a small community located in Southern California, and is A physics-based model of also situated along the San Andreas fault. The Parkfield segment of the earthquake cycle helps to assess the full range of the fault has frequently experienced strong earthquakes throughout seismic behavior that can history, and this Earthquake Physics project analyzes the unusual be expected across a plate tectonics behavior observed in this region. boundary. Earthquakes usually occur after a fixed period. However, the seismic history at Parkfield shows a series of tremors at irregular intervals. The research team led by Sylvain Barbot developed a unique simulation model, with significant contributions from Deepa Mele Veedu, that reproduces the Parkfield tremor activity including one thousand events, and is using this model to zero in on their study of earthquake recurrence patterns. The broad goal in this area of EOS research is to RESEARCH # increase fundamental knowledge of the region’s tec- 2–9 tonic and seismic behavior, as a basis for more reli- able forecasting of earthquakes and tsunamis as well as actions to reduce the potential hazards. 20 21 Earthquake Physics Sumatra Geodesy Project Tsunami Heights and Sediment Deposits Emma Hill Huang Zhenhua

Combining multiple The goal of Huang Zhenhua’s project geodetic data sets helps is to understand the source of a to separate the different signals in the data, and to tsunami from collecting and analyzing provide better-constrained sediment deposits in coastal caves models for earthquakes by investigating them through and sea-level change. laboratory experiments. Tsunami Zhenghua’s team found deposits are formed when tsunami that slip distribution, waves propagate in the inland area. geometry of the tsunami source, bathymetry, and The features of tsunami deposits, directivity affect the extent such as spatial distribution, thickness, of near-shore tsunamis. They also discovered RESEARCH # The Indonesian island of Sumatra is an area with high seismic and grain size, are indicative of that the landward extent activity. This is why EOS scientists and engineers have installed the features of tsunami waves. His 98 and elevation of tsunami the 60-station Sumatra GPS Array (SuGAr) to monitor seismic research employs a combination of deposits are indicative of behavior. Data obtained from GPS signals transmitted during numerical modelling, hydraulic lab tsunami size. seismic activities helps them understand the processes and hazards testing, as well as field observations, associated with active tectonics in the area. The Geodesy Group to investigate actual tsunami events. traces the behaviour patterns of the Mentawai seismic gap and Numerical experiments are then segments of the Sunda megathrust that may potentially cause a used to relate characteristics of the large earthquake in the near future. The team also keeps track of sediment deposition in a cave to the slip patterns of the Great Sumatran Fault, the seismic behavior in tsunami source. With the information the aftermath of large earthquakes, as well as the megathrust’s derived from tsunami deposits, we can potential for seismic and tsunami activity. With the GPS data, they better understand the locations and can also calculate the possibility of an earthquake’s occurrence nature of the source earthquakes that and whether the megathrust experiences gradual plate movement. generate tsunami waves. RESEARCH # The information gathered gives scientists insight into impending earthquakes and tsunamis that may occur in the region. 95

22 23 Geodesy Tsunami Modeling The Ratu River Expedition Volcano Research Judith Hubbard

Nepal is home to the Himalayas, which continue to grow as the Indian and Eurasian plates converge. This motion occurs along the Main Frontal Thrust, a fault that has recently been identified as the cause of the highly destructive 1934 Nepal earthquake. Judith Hubbard and the structural geology team embarked on an expedition to the Ratu River - which crosses the fault and is exposed during the dry season - to find out what the fault looks like beneath the Earth’s surface. The team uses an EnviroVibe seismic truck, as well as a set of 264 geophones, to detect ground vibrations that pass through the subsurface. The scientists collect the data in the field, then process and analyze it in the lab to visualize the Earth’s subsurface. The researches then match the seismic data to field observations, such as bedding planes or rock deposits. Members A close up of the mecha- Top of page: Understanding the shape of the fault எரிமலை of the team take a photo nism that vibrates the with the newly arrived six- ground to produce sound allows the scientists to predict how slip on ton seismic truck. waves for visualizing the the fault in an earthquakes should deform underground rock layers. 火山 the Earth’s surface, and therefore to translate the record of ground deformation into an Gunung Berapi estimate of slip in past events. Learning about the past behavior of this fault system is key to forecasting how it may behave in the future. The EOS Volcano Group conducts geologic, geochemical and geophysical studies to improve understanding of volcanic

RESEARCH # activity, particularly processes related to eruptions. They aid in forecasting volcanic eruptions, assessing their environmental 29–47–89 and societal impacts, and mitigating risk.

24 25 Structural Geology Monitoring of Volcanoes Assessing Hazards from with Infrasound Sumatran Volcanoes Taisne Caroline Bouvet

Among the 130-odd volcanoes in Sumatra, Indonesia, only a few have been studied by geologists. What makes investigating these volcanoes important is their close proximity to the 47 million inhabitants of the Indonesian island. Caroline Bouvet’s research assesses both active and potentially active volcanoes, their morphologies, and eruptive activities—identifying those with a high potential to erupt frequently and explosively—in Benoit Taisne, standing Benoit Taisne’s Lab Volcanoes’ project aims to understand the order to understand unrest signals in the middle, sets up a timing, rates and other details of the magma supply for different and forecast eruptions. This is temporary infrasound sen- sor with his team at Bukit volcanoes in order to improve forecasts of future eruptions. accomplished by employing Timah Nature Reserve Hundreds of volcanoes surround Singapore, and these methods that involve examining (L to R): Sorvigenaleon volcanoes are natural sources of infrasound. This project aims to the sediment strata of volcanoes, Ramos from the Technical Office, Corentin Caudron, detect and classify recorded infrasound signals during a volcanic their shapes and forms, as well as Sumatran volcanoes and Benoit, and Patrick Whel- explosion. Infrasounds are atmospheric low-frequency sounds focused studies of their locations. population density. Study- ley. ing Sumatra’s volcanic below the 20 Hz threshold of human hearing. They are generated Insight into the characteristics and activity and accessing during the explosive release of magma and gas, and can be recurrence of a volcano’s eruption eruption hazards in order recorded at large distances making them a robust indicator can be gained by referencing to set recovery plans in motion. that an eruption has occurred. In Singapore, this technology is the history of eruptions. These Details of the acquisition particularly interesting to detect, locate and characterize major methods can address the eruptive system for one point. From remote volcanic eruptions. The team’s first infrasound array in activity of Sumatra as a whole, left to right: digitizer and Singapore is set up at the MacRitchie Nature Reserve. initiating investigation of key data transmission, sensor and battery. The full infra- locations. sonic array is composed of five similar setups.

RESEARCH # RESEARCH # 85 14

26 27 Lab Volcanoes Physical Volcanology and Petrology Art+Media Research Isaac Kerlow

The Art+Media Group explores innovative methods for communicating Earth science to a wide audience. This group is also focused on raising the level of community engagement and regional preparedness that can ultimately lead to safer and more sustainable societies. The interdisciplinary projects developed and produced by this team involve research in the areas of storytelling, interactive media, film and animation. Earth Girl 2: Preparing for the Tsunami is an interactive casual strategy game about making strategic decisions that can directly increase the survival rate in At the market, players hear coastal communities during earthquake and a variety of opinions about tsunami scenarios. Earth Girl is the host and tsunamis. They must use guide, and the player is the protagonist. their judgment to distin- guish between fact and The game was developed by an fiction. interdisciplinary team of game artists Players can explore each and scientists at the Earth Observatory of level in the iPad App, Singapore. Earth Girl 2 is based on real-life looking for weak spots situations, with an emphasis on learning that can be enhanced with selected tools. The strate- preparedness and survival skills. It was gies laid out by the player inspired by the kids who live in coastal drive a crowd simulation communities throughout Asia, and by the interactive system. stories told by survivors of recent tsunamis.

Students at an elementary school in Padang, Indone- sia, collaborate and learn about tsunami prepared- ness using the Earth Girl 2 RESEARCH # casual strategy game. 35–36–37–38

28 29 www.earthgirl2.com www.earthgirl2.com Monitoring Hazards Paramesh Banerjee

GPS Networks The Sumatran GPS Array, SuGAr, is a network of 60 GPS stations Lab Volcanoes The Technical Office at Most of the SuGAr GPS EOS works closely with stations are installed in re- that spans more than a thousand kilometers along the convergent The Observatory’s volcano-monitoring local authorities, research mote locations throughout boundary between Indo-Australian and Asian tectonic plates. facilities enable fundamental research on and educational institu- Sumatra and the Menta- SuGAr is the most extensive of all the Observatory’s field-monitoring volcanoes at the Mayon volcano in Luzon, tions both in Singapore wai Islands, in Indonesia and overseas in its (see pages 46–47). efforts, and it is maintained by the Technical Office lead by Paramesh Philippines, and the Gede-Salak volcano in monitoring efforts. The Banerjee. Most of the stations are in Sumatra, directly above the West Java, Indonesia. The Technical Office observatory has invested Sunda megathrust, the giant fault that produced great earthquakes in staff maintains the equipment and the in a variety of modern ex- perimental, laboratory and the 2000s. The tsunami triggered by the 2004 earthquake killed about Volcano scientists lead the research projects monitoring instruments to 250,000 people in India, Thailand and Sumatra. that utilize the sensors. The Lab Volcanoes gather essential data for The Myanmar-Bangladesh-Assam GPS Network comprises 22 are aimed at understanding the timing, its research projects. Field monitoring relies primar- GPS stations and it monitors the ongoing collision of two of Earth’s rates and other specifics of the magma ily on networks of GPS, continental plates–the Indo-Australian and Eurasian plates. This supply of different volcanoes, in order to seismic and ultrasound is the site where some of the Earth’s greatest earthquakes have improve forecasts of future eruptions. instruments. occurred over the past few centuries.

30 31 Monitoring Hazards Monitoring Hazards Sustainability Education and Outreach Andreas Schaffer Susan Eriksson

The Sustainability Group works with government agencies and private sector organisations in the region to apply geo-hazards knowledge in projects such as infrastructure development, disaster resilience planning and climate change adaptation. Against the backdrop of a rapidly developing Southeast Asia, the Sustainability Group acts as a bridge, broker and catalyst to fulfil EOS’s mission of achieving safer and more sustainable societies in and around the region. The group also serves as a EOS contributed to the commercial transfer function for development of Earth science exhibits at the Sin- EOS – generating economic value gapore Science Centre. The goal of the in Singapore by providing world Sustainability Group is to harness geo-science class market oriented geo-hazards The Education and Outreach department works with internal Top left: EOS volcan- for safer livelihoods and solutions through three avenues: ologists and educators to safeguard economic and external media to build public’s awareness in Earth science geo-hazard assessments and brought teachers on a field assets in the region. research. Some of the outreach efforts include engaging informal seminar to Mount Merapi, The group identifies the technical consultancy services; education, field seminars, and museum exhibits. Indonesia. needs and strategies of provision of technological solutions international organizations EOS volcanologists and educators took 27 teachers from through partner organisations; and and governments and Singapore on field seminars at the Batur and Toba volcanoes in develops for them facilitation of multi-stakeholder Indonesia. These field experiences, including workshops before and customized solutions for workshops and programmes. geo-risk mitigation and after the trip, aimed to deepen the teachers’ content knowledge of sustainability. plate tectonics and volcanoes in Southeast Asia and their impact on people. The trips also sought to enhance teachers’ skills in designing and facilitating inquiry-based learning so that secondary students may benefit from it. The teachers’ evaluations were highly encouraging, with many considering this a valuable professional development. Many have incorporated this learning in their RESEARCH # classroom teaching and shared it with their colleagues, and that 27–74 their students are benefiting as a result.

32 33 Sustainability Education and Outreach Degree Programs Charles Rubin

The Division of Earth Sciences (DES) was founded in 2011 as the academic arm of the Earth Observatory of Singapore (EOS). Renamed as the Asian School of the Environment (ASE) it first offered a PhD in Earth Sciences, and later a Bachelor of Earth Systems students Science degree in Environmental Earth forged friendships over Systems Science, as well as a minor in food as they share a laugh with researcher and faculty Environmental Sustainability open to all memberJudith Hubbard. NTU students. The pioneer cohort of students comes from a variety of personal and academic backgrounds. These students work with professors, visiting scholars, and researchers from over 20 different countries and ten different fields.

Students pose for a photo It was a fun-filled evening with Charles Rubin, Head at the students’ welcome of NTU’s new Asian School barbecue as students of the Environment. made new friends to see them through the fresh- man year.

34 35 Degree Programs Degree Programs n Climate 07. Cartwright, J. A., U. Ott, D. W. Mittlefehldt, Jason Herrin, S. Herrmann, S. A. Mertz- Research Documents n Tectonics man, K. R. Mertzman, Z. X. Peng, and J. n Volcano E. Quinn. “The quest for regolithic howar- n dites. Part 1: Two trends uncovered using 2013/2014 Art+Media noble gases.” Geochimica et Cosmochimica n Applied Acta 105 (2013): 395-421. 08. Chakraborti, Dipankar, Mohammad Mah- mudur Rahman, Matthew Murrill, Reshmi Das, S. G. Patil, Atanu Sarkar, Dadapeer H.J, Saeed Yendigeri, Rishad Ahmed et al. List of research authored by principal Research Fellows 01. Andujar, Joan, Fidel Costa, and Bruno “Environmental arsenic contamination and investigators, research fellows, staff members, Scaillet. “Storage conditions and eruptive its health effects in a historic gold mining Annette Bolton: 3, 4, 57, 58 and PhD students at the Earth Observatory dynamics of central versus flank eruptions area of the Mangalur greenstone belt of Chiang Hong Wei: 54, 92 in volcanic islands: The case of Tenerife of Singapore roughly between January 2013 Northeastern Karnataka, India.” Journal of (Canary Islands, Spain).” Journal of Volcan- Hazardous Materials (2013). and May 2014. Reshmi Das: 8, 17 ology and Geothermal Research 260 (2013): 09. Chang, S.-H., J.-P. Avouac, Sylvain Barbot, Feng Lujia: 53, 67, 76 62-79. and J.-C. Lee. “Evidence for near-surface Christos Gouramanis: 24, 25, 43, 82, 87, 93, 96 02. Barbot, Sylvain, P. Agram, and M. De enhanced rate-strengthening derived from Michele. “Change of Apparent Segmenta- He Shaoneng River: 69 dynamic modeling of aseismic slip due to Principal Investigators tion of the San Andreas Fault Around Park- the 2004 Parkfield earthquake.” Journal of Iwan Hermawan: 72 field from Space Geodetic Observations Sylvain Barbot: 2, 9, 49 Geophysical Research (2013). Jason Scott Herrin: 7, 15, 16, 30, 70, 84, 86 Across Multiple Periods.” Journal of Geo- 10. Chen, J., Huang Z. H., Jiang C., Deng B., Caroline Bouvet Maisonneuve: 14, 66 physical Research: Solid Earth (in press) and Long Y. “Tsunami-Induced Scour at Dannie Hidayat: 26, 53 Fidel Costa: 1, 14, 23, 30, 32, 59, 63 (2013): 2013JB010442. Coastal Roadways: A Laboratory Study.” Li Lin Lin: 45, 46 03. Bolton, Annette, and Julene P. Marr. “Trace Natural Hazards, no. 69 (2013): 655-674. Nathalie Goodkin: 4, 64, 94 element variability in crust-bearing and non Kenneth Macpherson: 53 11. Cheng, Hai, Ashish Sinha, Francisco W. Emma Hill: 98 crust-bearing Neogloboquadrina incompta, Cruz, Xianfeng Wang, Lawrence R. Ed- Pradeep Venkata Mandapaka: 21, 55, 56 Huang Zhenhua: 10, 28, 45, 46, 95 P--D intergrade and Globoconella inflata wards, Fernando M. d’Horta, Camila C. Patrick Martin: 18, 20, 60, 61, 62 from the Southwest Pacific Ocean: Potential Ribas, Mathias Vuille, Lowell D. Stott, and Judith Hubbard: 29, 47, 89 paleoceanographic implications.” Marine Augusto S. Auler. “Climate change pat- Aron Meltzner: 5, 42 Isaac Kerlow: 34, 35, 36, 37, 38 Micropaleontology 100 (2013): 21-33. terns in Amazonia and biodiversity.” Nature Jeremy Pile: 13, 97 04. Bolton, Annette, Nathalie Goodkin, K. A. Communications 4 (2013): 1411. Koh Tieh-Yong: 39, 48 Teo Chee Kiat: 39 Hughen, Dorinda Ostermann, T. S. Vo, and 12. Cheng, Hai, R. Lawrence Edwards, Chuan- Mikinori Kuwata: 40, 68, 75 K. H. Phan. Paired Porites coral Sr/Ca and Chou Shen, Victor J. Polyak, Yemane Wang Yu: 91, 92 Qin Xiaosheng: 31, 50, 51, 52, 55 18O from the western South China Sea: Asmerom, Jon Woodhead, John Hellstrom, Patrick Whelley: 65 Proxy Calibration of Sea Surface Tempera- Yongjin Wang, Xinggong Kong, Christoph Charles Rubin: 24 ture and Precipitation (in press). Christina Widiwijayanti: 71 Spötl, Wang Xianfeng and E. Calvin Alex- Kerry Sieh: 5, 91, 92, 98 05. Bursik, M., Kerry Sieh, and Aron Meltzner. ander Jr. “Improvements in 230Th dating, Yu Fengling: 78, 82, 96, 97 “Deposits of the most recent eruption in Adam Switzer: 24, 25, 43, 65, 79, 80, 81, 82, 230Th and 234U half-life values, and U-Th 83, 96, 97 the Southern Mono Craters, California: isotopic measurements by multi-collector Description, interpretation and implications inductively coupled plasma mass spec- Benoit Taisne: 85 PhD Students for regional marker tephras.” Journal of trometry.” Earth and Planetary Science Paul Tapponnier: 44, 73 Társilo Girona: 23 Volcanology and Geothermal Research, no. Letters 371-372 (2013): 82-91. 275 (2014): 114-131. Cooper, J. A. G., and Jeremy Pile. “The Wang Xianfeng: 11, 12, 19, 22, 77, 88, 90 Sujata Annavarapu Murty: 41 13. 06. C. Chamberlain, Page, Xiaoqiao Wan, adaptation-resistance spectrum: A clas- Pham Tien Dat: 24, 43, 82 Stephan A. Graham, Alan R. Carroll, Amalia sification of contemporary adaptation Staff Qiu Qiang: 46 C. Doebbert, Bradley B. Sageman, Peter approaches to climate-related coastal Blisniuk, Malinda Kent-Corson, Zhou Wang, change.” Ocean & Coastal Management 94 Malinda Kent-Corson: 6, 33 Sim Yisheng Shawn: 28 and Wang Chengshan. “Stable isotopic (2014): 90-98. Dorinda Ostermann: 4 Janneli Lea Acierto Soria: 43, 82 evidence for climate and basin evolution of 14. Costa, Fidel, Supriyati Andreastuti, Caroline the Late Cretaceous Songliao basin, China.” Andreas Schaffer: 27, 74 Yang Teng Teng: 94 Bouvet de Maisonneuve, and John S. Pal- Palaeogeography, Palaeoclimatology, Pal- lister. “Petrological insights into the storage aeoecology 385 (2013): 106-124. conditions, and magmatic processes that

36 37 Research Documents Research Documents n Climate n Tectonics n Volcano n Art+Media n Applied Azurite Cu (Co ) (OH) Galena, PbS 3 3 2 2 Fluorite, CaF2 An Hui, China Missouri, USA Coahuila, Mexico

yielded the centennial 2010 Merapi explo- semble nowcasting of orographic rainfall.” Change and Food Security. Bandung, Indo- Science. Earth Observatory of Singapore. sive eruption.” Journal of Volcanology and Meteorological Applications (2014). nesia, 2013. Singapore, 2014. ISBN 978-981-07-9659-4. Geothermal Research 261 (2013): 209-235. 22. Frappier, A., J. Pyburn, A. Pinkey-Drobnis, 28. Huang Z. H., Wu T.-R., Chen T.-Y., Sim S. Y. 35. Kerlow, Isaac. “Computer Games for Chil- 15. D. Lever, G. Jones, and J. Herrin. “Compar- Xianfeng Wang, D.R. Corbett, and B.H. “A Possible Mechanism of Destruction of dren in Natural Hazard Areas.” Asia-Pacific ing the precision of two analytical methods Dahlin. “Two millennia of tropical cyclone- Coastal Trees by Tsunamis: A Hydrodynam- Science, Technology and Society Network for determining boron in glass – a statisti- induced mud layers in a northern Yucatan ic Study on Effects of Coastal Steep Hills.” (APSTSN) Biennial Conference 2013. Singa- cal approach using Gage R&R.” 2014. Glass stalagmite reveal multiple overlapping Journal of Hydro-environment Research 7 pore, 2013. Technology: European Journal of Glass Sci- climatic hazards during the Terminal Clas- (2013): 113-123. 36. Kerlow, Isaac. “Earth Girl: A Game of Aware- ence and Technology. 55(3):73-80. 2013. sic Period Megadroughts.” Geophysical 29. J. Hubbard, J. H. Shaw, J. Dolan, T. L. Pratt, ness and Survival. Games for Change 16. D. W. Mittlefehldt, J. S. Herrin, J. E. Quinn, Research Letters (2014). L. McAuliffe, and T. K. Rockwell. “Structure Europe, FMX. Stuttgart, Germany, 2013. S. A. Mertzman, J. A. Cartwright, K. R. 23. Girona, Tarsilo, and Fidel Costa. “DIPRA: A and seismic hazard of the Ventura Avenue 37. Kerlow, Isaac. “Indigenous Legends in Mertzman, and Z. X. Peng. “Composition user-friendly program to model multi-ele- anticline and Ventura fault, California: Pros- the Context of Contemporary Storytell- and petrology of HED polymict breccias: ment diffusion in olivine with applications pect for large, multi-segment ruptures in ing.” 20th Stuttgart International Festival The regolith of (4) Vesta.” 2013. Meteoritics to timescales of magmatic processes.” the Western Transverse Ranges.“ BSSA, vol. of Animated Film; Symposium on Change and Planetary Science 48 (11): 2166-2184. Geochemistry, Geophysics, Geosystems 104 (3) (2014): 1070-1087. and Continuity: Interdisciplinary Aspects of 17. Das, Reshmi, Michael Bizimis, and Alicia M. 14, no. 2 (2013): 422-431. 30. Jay J., Costa F., Pritchard M., Lara L., Animation, Comics and Literature. Stutt- Wilson. “Tracing seawater vs. at- 24. Gouramanis, Chris, A. D. Switzer, C. Bris- Singer B., Herrin, J. “Locating magma res- gart, Germany, 2013 (in press). mospheric inputs in a pristine SE USA salt tow, K. Jankaew, Charles M. Rubin, D.T. ervoirs using InSAR and petrology before 38. Kerlow, Isaac. “Using Computer Games for marsh system: Mercury isotope evidence.” Pham, and Y. S. Lee. “Thin-bed Ground- and during the 2011–2012 Cordón Caulle si- Effective Awareness and Preparedness.” Chemical Geology 336 (2013): 50-61. Penetrating Radar analysis of preserved licic eruption.” Earth and Planetary Science Asia Oceania Geosciences Society (AOGS) 18. Decelle, J., Patrick Martin, K. Pabortsava, modern and palaeotsunami deposits from Letters (2014). 395: 254–266. 11th International Conference. Brisbane, R.S. Lampitt, G. Tarling, D. Pond, and F. Not. Phra Thong Island, Thailand.” Proceedings 31. J., Yu J., Xiaosheng Qin, and O. Larsen. Australia, 2013. “Phylogeny and biogeography of cyst- of the 15th International Conference on “Joint Monte Carlo and possibilistic 39. Koseki, Shunya, Tieh-Yong Koh, and Chee- forming Acantharia (Radiolaria) shed light Ground Penetrating Radar (in press). simulation for flood damage assessment.” Kiat Teo. “Effects of the cold tongue in the on their ecology and biogeochemistry in the 25. Gouramanis, Chris, Patrick De Deckker, Stochastic Environmental Research and South China Sea on the monsoon, diurnal oceans.” PLoS ONE 8, no. e53598 (2013). Adam Switzer, and Daniel Wilkins. “Cross- Risk Assessment 27, no. 3 (2013): 725-735. cycle and rainfall in the Maritime Conti- 19. Duan, F.C., D.B. Liu, H. Cheng, Xianfeng continent comparison of high-resolution 32. Kahl, Maren, Sumit Chakraborty, Fidel nent.” Quarterly Journal of the Royal Mete- Wang, Y.J. Wang, X.G. Kong, and S.T. Chen. Holocene climate records from southern Costa, Massimo Pompilio, Marco Liuzzo, orological Society 139 (2013): 1566-1582. “A high-resolution monsoon record of Australia-Deciphering the impacts of and Marco Viccaro. “Compositionally 40. Kuwata, M., W. Shao, R. Lebouteiller, and millennial-scale oscillations during Late far-field teleconnections.” Earth-Science zoned crystals and real-time degassing S. T. Martin. “Classifying organic materi- MIS3 from Wulu Cave, south-west China.” Reviews 121 (2013): 55-72. data reveal changes in magma transfer als by oxygen-to-carbon elemental ratio Journal of Quaternary Science 29, no. 1 26. Hautmann, S., Dannie Hidayat, N. Fournier, dynamics during the 2006 summit eruptive to predict the activation regime of cloud (2014): 83-90. A. T. Linde, I. S. Sacks, and C. P. Williams. episodes of Mt. Etna.” Bulletin of Volcanol- condensation nuclei (CCN).” Atmos. Chem. 20. F., Ebersbach, P. Assmy, Patrick Martin, I. “Pressure changes in the magmatic system ogy 75 (2013): 1-14. Phys. 13 (2013): 5309-5324. Schulz, S. Wolzenburg, and E.-M. Nöthig. during the December 2008/January 2009 33. Kent-Corson, Malinda, Anthony D. Barnos- 41. Lamborg, Carl H., Gretchen Swarr, Konrad “Particle flux characterisation and sedi- extrusion event at Soufriere Hills Volcano, ky, Andreas Mulch, Marc A. Carrasco, and Hughen, Ross J. Jones, Scot Birdwhistell, mentation patterns of protistan plankton Montserrat (W.I.), derived from strain data Page C. Chamberlain. “Possible regional Kathryn Furby, Sujata Annavarapu Murty, during the iron fertilisation experiment analysis.” Journal of Volcanology and Geo- tectonic controls on mammalian evolution Nancy Prouty, and Chun-Mao Tseng. LOHAFEX in the Southern Ocean.” Deep- thermal Research 250 (2013): 34-41. in western North America.” Palaeogeogra- “Determination of low-level mercury in Sea Research Part I, no. 89 (2014): 94-103. 27. Hoh, Edmund W. M., and Andreas Schaffer. phy, Palaeoclimatology, Palaeoecology 387 coralline aragonite by calcination-isotope 21. Foresti, Loris, Luca Panziera, Pradeep V. “The Valuation of Conservation Options (2013): 17-26. dilution-inductively coupled plasma-mass Mandapaka, Urs Germann, and Alan Seed. Versus Tropical Deforestation.” In Interna- 34. Kerlow, Isaac, ed. The EOS ART Projects spectrometry and its application to Diploria “Retrieval of analogue radar images for en- tional Conference on Biodiversity, Climate 2010-2013, Six Art Projects Inspired by Earth specimens from Castle Harbour, Bermuda.”

38 39 Research Documents Research Documents Tourmaline 2+ n Climate NaFe 3Al6Si6O18(BO3)3(OH)3OH Minas Gerais, Brazil n Tectonics Barite, Ba(SO ) 4 n Volcano Nevada, USA (Opposite page) n Art+Media n Applied

Geochimica et Cosmochimica Acta 109 54 (2013): 199-214. Qin. “Analysis and characterization of prob- tion enhanced net community production (2013): 27-37. 48. Li, Xian-Xiang, Tieh-Yong Koh, Dara En- ability distribution and small-scale spatial but not downward particle flux during the 42. Lee, Jong-Mi, Edward A. Boyle, Intan Suci tekhabi, Matthias Roth, Jagabandhu Panda, variability of rainfall in Singapore using a Southern Ocean iron fertilization experi- Nurhati, Miriam Pfeiffer, Aron Meltzner, and Leslie K. Norford. “A multi-resolution dense gauge network.” Journal of Applied ment LOHAFEX.” Global Biogeochemical and Bambang Suwargadi. “Coral-based ensemble study of a tropical urban en- Meteorology and Climatology 52 (2013): Cycles 27 (2013): 871-881. history of lead and lead isotopes of the vironment and its interactions with the 2781-2796. 62. Martin, Patrick, S.T. Dyhrman, M.W. Lo- surface Indian Ocean since the mid-20th background regional atmosphere.” Journal 56. Mandapaka, Pradeep V., U. Germann, and mas, N.J. Poulton, and B.A.S. Van Mooy. century.” Earth and Planetary Science Let- of Geophysical Research: Atmospheres 118 L. Panziera. “Diurnal cycle of precipitation “Accumulation and enhanced cycling of ters 398 (2014): 37-47. (2013): 9804-9818. over complex Alpine orography: inferences polyphosphate by Sargasso Sea plankton 43. Lee, Y. S., Chris Gouramanis, Adam Switzer, 49. Lindsey, E. O., V. J. Sahakian, Y. Fialko, Y. from high-resolution radar observations.” in response to low phosphorus.” Proceed- CS. Bristow, Lea Soria, Dat Pham, DD. Lam, Bock, Sylvain Barbot, and T. K. Rockwell. Quarterly Journal of the Royal Meteoro- ings of the National Academy of Sciences, and Que HD. “Ground penetrating radar “Interseismic strain localization in the San logical Society 139 (2013). no. 111(22) (2014): 8089-8094. (GPR) survey of formerly mined coastal Jacinto fault zone.” Pure and Applied Geo- 57. Marr, Julene P., Helen C. Bostock, Lionel 63. Marzoli, A., Jourdan F., Bussy F., Chiaradia sand in central Vietnam: a rapid, non-inva- physics (2013): 1-18. Carter, Annette Bolton, and Euan Smith. M., Costa F. “Petrogenesis of tholeiitic sive method for investigating the extent and 50. Lu, Y., and Xiaosheng Qin. “A coupled K- “Differential effects of cleaning procedures basalts from the Central Atlantic magmatic impact of mined areas.” Journal on Geologi- Nearest Neighbor and Bayesian Neural Net- on the trace element chemistry of plank- province as revealed by mineral major and cal and Earth Sciences 1 (2013): 36-45. work model for daily rainfall downscaling.” tonic foraminifera.” Chemical Geology 351 trace elements and Sr isotopes.” Lithos 44. Leloup, P. H., R. F. Weinberg, B. K. Mukher- International Journal of Climatology (2013). (2013): 310-323. (2014) 188: 44-59. jee, Paul Tapponnier, R. Lacassin, E. Bou- 51. Lu, Y., and Xiaosheng Qin. “Multisite rain- 58. Marr, Julene P., Lionel Carter, Helen C. 64. N. Prouty, Grumet, Nathalie Goodkin, C. tonnet, M. L. Chevalier, F. Valli, H. Li, N. fall downscaling and disaggregation in a Bostock, Annette Bolton, and Euan Smith. H. Lamborg, R. Jones, and K. A. Hughen. Arnaud et al. “Comment on “Displacement Tropical Urban Area.” Journal of Hydrology “Southwest Pacific Ocean response to a “Environmental Assessment of Metal Ex- along the Karakoram fault, NW Himalaya, 509 (2014): 55-56. warming world: Using Mg/Ca, Zn/Ca, and posure to Corals Living in Castle Harbour, estimated from LA-ICP-MS U-Pb dating 52. Lu, Y., Xiaosheng Qin, and T. Y. Xu. “Sta- Mn/Ca in foraminifera to track surface Bermuda.” Marine Chemistry (2013). of offset geologic markers” published by tistical downscaling and disaggregation ocean water masses during the last de- 65. Paris, R., Adam Switzer, M. Belousova, Shifeng Wang et al. in EPSL, 2012.” Earth of rainfall using a master-station-based glaciation.” Paleoceanography 28 (2013): A. Belousov, B. Ontowirjo, P. 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40 41 Research Documents Research Documents locked plate interface.” Nature Geoscience and Andrew Newman. “Long-term versus n Climate 7, no. 2 (2014): 117-121. short-term deformation of the meizoseis- 68. Renbaum-Wolff, L., J. Grayson, A. Bate- mal area of the 2008 Achaia-Elia (MW 6.4) n Tectonics man, M. Kuwata, M. Sellier, B. J. Murray, J. earthquake in NW Peloponnese, Greece: n Volcano E. Shilling, S. T. Martin, and A. K. Bertram. Evidence from historical triangulation and n “Viscosity of ALPHA-pinene secondary or- morphotectonic data.” Tectonophysics 592 Art+Media ganic material and implications for particle (2013): 150-158. n Applied growth and reactivity.” Proc. Natl. Acad. 77. Stoll, H., A. Moreno, A. Mendez-Vicente, S. Sci. USA. (2013). Gonzalez-Lemos, Jimenez -Sanchez, M.J. Quarz, SiO2 69. Robert G. Walsh, Shaoneng He, and Chris- Dominguez-Cuesta, R.L. Edwards, H Cheng, Colombia topher T. 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T. , and Nathalie Goodkin. “Wet ing Aisyah, Christina Widiwijayanti, and ods and techniques for the modern geomor- in the Red River Delta using remotely Season Upwelling and Dry Season Chloro- Philippe Jousset. “Interpretation of ground phologist: an introduction to the volume.” sensed data.” Journal of Marine Science phyll-a Describe Inter-Annual Growth Rates surface changes prior to the 2010 large In Treatise on Geomorphology, 1-5. Vol. 14. and Technology 13, no. 2 (2013): 151-160. of Porites in Southern China.” PLoS ONE 9, eruption of Merapi volcano using ALOS/ San Diego, CA: Academic Press, 2013. 88. WAIS Divide Project Members, T. J. Fudge, no. 6 (2014): e99088. PALSAR, ASTER TIR and gas emission 80. Switzer, Adam, and D. M. Kennedy. E. J. Steig, B. R. Markle, S. W. Schoene- 95. Yao Yao, Z. H. Huang, Edmund Y. M. Lo, and data.” Journal of Volcanology and Geother- “Techniques and methods for the field: an mann, Q. Ding, K. C. Taylor, J. R. 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Yu, Fengling, Adam Switzer, An Yi Annie Nature Geoscience 6 (2013): 71-76. of Coastal Research, no. 70 (2014): 723-729. “Long-term reworking of volcanic ash de- Lau, Hoi Yan Esther Yeung, Shun Wah Chik, 74. Schaffer, Andreas. “24.9.1. Transboundary 83. Switzer, Adam. “Laboratory techniques posited in the abyssal ocean based on ura- Hon Chim Chiu, Zhaoquan Huang, and Jer- Adaptation Planning and Management - for geomorphologists: an introduction.” In nium and thorium measurements.” Journal emy Pile. “A comparison of the post-storm Lower Mekong River Basin.” In Intergovern- Treatise on Geomorphology, 222-223. Vol. of Volcanology and Geothermal Research recovery of two sandy beaches on Hong mental Panel on Climate Change (IPCC) 5th 14. San Diego, CA: Academic Press, 2013. 264 (2013): 66-71. Kong Island, southern China.” Quaternary Assessment Report- Asia Chapter. Intergov- 84. T. Baikie, M. K. Schreyer, F. Wei, J. S. Herrin, 91. Wang, Yu, Kerry Sieh, S. T. Tun, K.-Y. Lai, International 304 (2013): 163-175. ernmental Panel on Climate Change, 2014. C. Ferraris, F. Brink, J. Topolska, R. Piltz, J. and T. Myint. “Active tectonics and earth- 98. Yue, H., T. Lay, L. , Y. Bai, Y. Yamazaki, 75. Smith, M. L., Y. You, M. Kuwata, A. K. Ber- Price, and T. J. White. “The Influence of quake potential of the Myanmar region.” K. F. Cheung, Emma Hill, Kerry Sieh, W. tram, and S. T. Martin. “Phase Transitions Stereochemically Active Lone Pair Elec- Journal of Geophysical Research: Solid Kongko, and A. Muhari. “Rupture process and Phase Miscibility of Mixed Particles trons on Crystal Symmetry and Twist An- Earth 119, no. 4 (2014): 3767-3822. of the 2010 Mw 7.8 Mentawai tsunami of Ammonium Sulfate, Toluene-Derived gles in Lead Apatite-2H Minerals.” Mineral- 92. Wang, Yu, Bruce J. H. Shyu, Kerry Sieh, earthquake from joint inversion of near- Secondary Organic Material, and Water.” ogical Magazine 78, No. 2 (2014): 325–345. Hong-Wei Chiang, Chung-Che Wang, Thura field hr-GPS and teleseismic body wave Journal of Physical Chemistry 117 (2013): 85. Tait, S., and Benoit Taisne. “Experimental Aung, Yu-nung Nina Lin, Chuan-Chou recordings constrained by tsunami obser- 8895-8906. models of hydraulic fissures with appli- Shen, Soe Min, Oo Than et al. “Permanent vations.” Journal of Geophysical Research: 76. Stiros, Stathis, Fanis Moschas, Lujia Feng, cation to the propagation of magmatic upper plate deformation in western My- Solid Earth 119 (2014).

42 43 Research Documents Research Documents Research Technology

Clean Room Specially designed, this metal-free chemistry clean Mass Spectrometer laboratory is used to prepare samples for mass IVI Envirovibe Truck spectrometric measurements. Equipped with a This state-of-the-art facility supports a variety dedicated air handling unit and HEPA filters, this lab The IVI Envirovibe is a seismic vibration of cutting-edge research in low-temperature exceeds Class 1,000 conditions. Features include a truck used to image subsurface faults geochemistry, climate, and environmental change main chemistry room containing five fume hoods, in places like Nepal, Bangladesh, and through high-precision isotope analyses, with an one horizontal laminar flow workstation, six working Myanmar, where EOS conducts research emphasis on isotopes of U, Th, Sr, Nd, Pb and Hg benches for sample digestions, chromatographic projects. This mammoth machine works by using an inductively-coupled plasma as a highly separations, and trace element purification. with a set of sensors detecting ground efficient ion source. Equipped with nine Faraday vibrations. The data is processed, cups and two ion counters for simultaneous isotope providing high-resolution seismic collection, it dramatically increases the overall reflection profiles that enable the EOS efficiency and precision of isotopic measurements. tectonics team to unravel fault behavior and fold growth in seismically active and densely populated regions.

Laser Ablation System Wave Glider LIDAR Scanner Boasting a precision of 1 to 400 micrometers, this system The Wave Glider is a The LIDAR scanner is an instrument determines trace amounts seagoing robot fitted that digitizes a site’s topography with of almost any chemical with sensors for sea exquisite precision. It measures the element. The presence of floor exploration that distance to a target by emitting light trace elements in certain monitors the Enggano pulses. This equipment is used to environments can provide and Mentawai segments map faults and earthquake rupture clues about the environmental Isotope Mass Spectrometer of the Sunda megathrust, offsets with an accuracy that allows conditions that existed during off southern Sumatra that researchers to constrain precisely their growth. Materials that This instrument measures the relative abundance could trigger earthquakes the slip-distribution of various are chemically analyzed at of isotopes in a given sample, for example, oxygen and tsunamis. Working faults in Asia. With complementary EOS with this instrument isotopes in coral skeletons. These ratios incorporated in conjunction with the dating, scientists can also estimate include igneous rock during the organism’s growth process are used as Sumatran GPS Array earthquake cycles on a given fault. crystals, speleothems, corals, an indicator for measuring sea surface temperature (SuGAr) and offshore Sedimentologists also use the LIDAR microfossils, fish otoliths and and salinity through time. The data acquired may networks, this instrument to precisely map various outcrops. scales, and organic tissues. allow scientists to determine climate and other helps EOS scientists environmental conditions that were present. understand potential hazards.

44 45 Research Technology Research Technology Research Projects 2013/2014

SINGAPORE [SG] MEXICO [MX]** 1 EOS ART Projects* 21 El Mayor Cucupah Isaac Kerlow [CN, PH, TH] Sylvain Barbot 2 Sea Level on Sunda* [ID] MYANMAR [MM] Adam Switzer 22 Surface Rupture 2011 Tarlay BANGLADESH [BD] Kerry Sieh 3 Dauki Fault 23 Uplift History Sunda Megathrust Judith Hubbard Kerry Sieh 4 Fold-and-Thrust Belt NEPAL [NP] Judith Hubbard 24 Characterizing the Sub-Surface CHINA [CN] Judith Hubbard 5 Altyn Tagh Fault 25 Knowledge Capsules Paul Tapponnier Isaac Kerlow 6 Fuyun Fault 26 Eastern Nepal NEPAL CHINA Paul Tapponnier Paul Tapponnier INDIA [IN] PAPUA NEW GUINEA [PG] 7 Bay of Bengal Climate 27 Magma Degassing Emma Hill Caroline Bouvet Maisonneuve 8 Bengal Assam BANGLADESH PHILIPPINES [PH] Paul Tapponnier TAIWAN 28 Plumbing System INDONESIA [ID] Fidel Costa 9 Mentawai Seismic Gap 29 Mayon Lab Volcano MYANMAR Sylvain Barbot Benoit Taisne 10 Stress Evolution TAIWAN [TW] Sylvain Barbot 30 Coral Geochemistry 11 Wave Glider Nathalie Goodkin Sylvain Barbot PHILIPPINES 12 Aftermath of AID THAILAND [TH] INDIA THAILAND Patrick Daly 31 Tracking Hydroclimate Variation* 13 Doangdoang Besar Island Wang Xianfeng [ID, MM] Nathalie Goodkin UNITED STATES [US]** 14 Banda Aceh Documentary 32 Parkfield Tremors Isaac Kerlow Sylvain Barbot 15 Earth Girl 2 Isaac Kerlow VIETNAM [VT] 16 Merapi Interactive 33 Coastal Hazards in Asia* [CN, Isaac Kerlow IN, PH, TH, TW] VIETNAM 17 Aceh Cave Adam Switzer Charles Martin Rubin 18 West Sumatra Education Andeas Schaffer 19 Sumatran Slip Rates Notes Kerry Sieh * Research carried out in INDONESIA multiple countries. SINGAPORE 20 Gede Salak Lab Benoit Taisne ** Not represented in this map. GPS NETWORKS A Sumatran GPS Array, SuGAr 60 stations, GREEN B Myanmar-Bangladesh-Assam PAPUA NEW GUINEA GPS Network 22 stations, blue

46 47 Prime Minister Lee Visit 2014 News Flash

Prime Minister Lee Hsien Loong visited EOS to learn about the Observatory’s research and new developments. PM Lee was given a tour of the facility, and had the opportunity to see the ongoing EOS projects. Principal investigators and group leaders presented their work to the Prime Minister in the areas of climate change in Southeast Asia, monitoring of volcano eruptions around Singapore, analysis of major faults in South Asia, a casual strategy interactive Technical Director Para- game about preparing for the tsunami, and mesh Banerjee (right) jokes with PM Lee and a cutting-edge monitoring network along the Minister for Education particularly seismically active Sumatra. Heng Swee Keat (left) as At the tea session after the main school tour, he shows them the LIDAR scanner that EOS scien- the Prime Minister exchanged thoughts with tists use in the field. international scientists and PhD students from around the world who have chosen to Fancy a hands-on approach make Singapore their home, and EOS their to learning? Here, faculty research center of choice. member and researcher Fidel Costa (left) shows After the visit, Prime Minister Lee PM Lee a volcanic rock reflected in a FaceBook post: “The world sample, which can give is so much more interesting when we are clues to a volcano’s erup- tive history. NTU President curious. Learned some fascinating facts Bertil Andersson (center) and developments on my visit to the Earth and Provost Freddy Boey Observatory of Singapore today. EOS seeks (far right) follow the dem- onstration with interest. to understand better how our dynamic planet works, to help us cope with natural disasters. It studies climate, volcanoes, Faculty member and earthquakes, and tsunamis.” researcher Koh Tieh Yong (left) uses the EOS Geo- Touch system to present climate trends to PM Lee.

48 49 Prime Minister Lee Visit Prime Minister Lee Visit Financial Statements Staffing 1 April 2013 – 31 2014 1 April 2013 – 31 March 2014

Total Assets* 30,811,438 Director’s Office 2 RESEARCH

Grants and Other 8,850,952 Receivables Climate Group 22 Net Funds Owed 7,624,605 from NTU

Total Current Assets 16,125,557 Tectonics Group 22.5

Funds Held on 11,761,407 behalf by NTU Volcano Group 12 Plant and 2,924,474 Equipment

Total Non-Current 14,685,881 * Cash on Hand: 10,000 Art+Media Group Assets 10

Total Liabilities, 30,811,438 Funds and Reserves Technical Office 11 SUPPORT Accrued Expenses and 2,067,047 Other Payables

Grants Received in 9,090,258 Sustainability Office Advance From NTU 4

Total Current 11,157,305 Liabilities Education and 8 Deferred Capital 2,924,474 Outreach Office Grant

Development Office Endowment Funds 11,761,407 1

Accumulated 4,968,252 Surplus Corporate Support Office 8 Total Funds and 16,729,659 Reserves

50 51 Financial Statements Staffing Credits

Photography Hermann Fritz, Lea 31. Juniator Tulius, Editorial Acierto Soria. Technical Office Team. Front Cover 12. Zhang Xiao, 32. Ankit Joshi. Editorial and Sorvigenaleon Ramos. Sutthirat Supaparinya, 33. Sylvain Lefèvre, Design Direction Back Cover Chen Sai Hua Kuan. Singapore Science Isaac Kerlow Corentin Caudron, 13. Robert Zhao Centre. Annette Bolton, Chen Renhui, Clara 34–43. Gel See Toh. Editorial Team MengLi, Jocelyn Balaguer, Isaac 44. Yvonne Soon, Tan Cheryl Han West, Sorvigenaleon Kerlow. Wenkai. Ng Huijia Ramos, Sujata Murty, 14. Chen MengLi. 45. Yvonne Soon, Isaac Kerlow Gel See Toh. 15. Joanne Petrina. Tong Junwei, Sylvain Page 2. Agathe 16. STR/AFP/Getty Barbot, Isaac Kerlow. Photo Coordination Schmid. Images. 46. Joanne Petrina, Yvonne Soon 3. Joanne Petrina. 17. Isaac Kerlow. Sorvigenaleon 4. Kerry Sieh, Isaac 18. Qin Xiaosheng. Ramos, Cagil Karakas, Staff Portraits Kerlow. 19. Koh Tieh Yong. Annie Winson, Paul Ang 5. Kerry Sieh, Isaac 20. Jocelyn West. Jocelyn West. Kerlow. 21. Sylvain Barbot, 47. Corentin Map 6. Paul Tapponnier, Deepa Mele Veedu. Caudron, Jocelyn Wang Xin Kate Ravillious 22. Feng Lujia. West. Rachel Goh 7. Paul Tapponnier, 23. Li Lin Lin. 48–49. Jean Humza Akhtar Cagil Karakas. 24. Isaac Kerlow. 25. Qingwen Loo. Jonah Yong 8. Sylvain Lefèvre, Corentin Caudron. 50. Agathe Schmid, Isaac Kerlow. 26. Sylvain Lefèvre. Aurélie Coudurier- 9. Fidel Costa, Isaac 27. Caroline Bouvet. Curveur. Kerlow. 28. Art+Media Team. 51. Aurélie 10. John Elton Chua, 29. Art+Media Team, Coudurier-Curveur, Angel Doctor. Isaac Kerlow. Agathe Schmid. 11. Yvaine Sta. Maria, 30. Agathe Schmid.

52 53 www.earthobservatory.sg www.earthobservatory.sg

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