On the Future of Argo: a Global, Full-Depth, Multi-Disciplinary Array
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Comparing Historical and Modern Methods of Sea Surface Temperature
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Open Access Open Access Climate Climate of the Past of the Past Discussions Open Access Open Access Earth System Earth System Dynamics Dynamics Discussions Open Access Geoscientific Geoscientific Open Access Instrumentation Instrumentation Methods and Methods and Data Systems Data Systems Discussions Open Access Open Access Geoscientific Geoscientific Model Development Model Development Discussions Open Access Open Access Hydrology and Hydrology and Earth System Earth System Sciences Sciences Discussions Open Access Ocean Sci., 9, 683–694, 2013 Open Access www.ocean-sci.net/9/683/2013/ Ocean Science doi:10.5194/os-9-683-2013 Ocean Science Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Solid Earth Solid Earth Discussions Comparing historical and modern methods of sea surface Open Access Open Access The Cryosphere The Cryosphere temperature measurement – Part 1: Review of methods, Discussions field comparisons and dataset adjustments J. B. R. Matthews School of Earth and Ocean Sciences, University of Victoria, Victoria, BC, Canada Correspondence to: J. B. R. Matthews ([email protected]) Received: 3 August 2012 – Published in Ocean Sci. Discuss.: 20 September 2012 Revised: 31 May 2013 – Accepted: 12 June 2013 – Published: 30 July 2013 Abstract. Sea surface temperature (SST) has been obtained 1 Introduction from a variety of different platforms, instruments and depths over the past 150 yr. -
BIOGRAPHRIES and ABSTRACTS from HMS Challenger to Argo And
BIOGRAPHRIES AND ABSTRACTS From HMS Challenger to Argo and Beyond - Introduction Prof Chris Folland, Met Office Abstract | The purpose of this introductory talk is first to welcome all speakers and participants followed by a brief mention of the backgrounds of the organisers, and how they relate to the topic of the meeting. The revolutionary nature of the ARGO program for oceanography, and climate applications in particular, will be emphasised helped by selected update to date information from the ARGO web site. Finally, the structure of the meeting will be summarised. I will then introduce the next speaker, John Gould. Biography | Professor Chris Folland headed the Met Office Hadley Centre’s Climate Variability and Seasonal Forecasting Group (1990-2008), retiring as a Research Fellow in 2017. Chris was a Lead Author for four reports of the Intergovernmental Panel on Climate Change (IPCC) where, like other Lead Authors, he shared in the Nobel Peace Prize awarded to IPCC in 2007. He has several fellowships and has won a number of national and international awards. Chris remains Honorary Professor at the University of East Anglia, Guest Professor of Climatology at the University of Gothenburg, Sweden and Adjunct Professor at the University of Southern Queensland, Australia. From thermometers to Robots - evolution and revolution Dr W John Gould, National Oceanography Centre Abstract | The talk will show how our ability to collect temperature and salinity profiles from the open ocean has developed starting with the early voyages of HMS Challenger and SMS Gazelle in the1870s, through the 1920s and 30s (Discovery Investigations and Meteor Expedition) to the 1940s and the invention of the bathythermograph. -
Report on Microbial Threats in the Arctic
THE NATIONAL ACADEMIES PRESS This PDF is available at http://nap.edu/25887 SHARE Understanding and Responding to Global Health Security Risks from Microbial Threats in the Arctic: Proceedings of a Workshop (2020) DETAILS 96 pages | 7 x 10 | PAPERBACK ISBN 978-0-309-68125-4 | DOI 10.17226/25887 CONTRIBUTORS GET THIS BOOK Lauren Everett, Rapporteur; Polar Research Board; Board on Life Sciences; Board on Global Health; Division on Earth and Life Studies; Health and Medicine Division; National Academies of Sciences, Engineering, and Medicine; FIND RELATED TITLES InterAcademy Partnership; European Academies Science Advisory Council SUGGESTED CITATION National Academies of Sciences, Engineering, and Medicine 2020. Understanding and Responding to Global Health Security Risks from Microbial Threats in the Arctic: Proceedings of a Workshop. Washington, DC: The National Academies Press. https://doi.org/10.17226/25887. Visit the National Academies Press at NAP.edu and login or register to get: – Access to free PDF downloads of thousands of scientific reports – 10% off the price of print titles – Email or social media notifications of new titles related to your interests – Special offers and discounts Distribution, posting, or copying of this PDF is strictly prohibited without written permission of the National Academies Press. (Request Permission) Unless otherwise indicated, all materials in this PDF are copyrighted by the National Academy of Sciences. Copyright © National Academy of Sciences. All rights reserved. Understanding and Responding to Global Health Security Risks from Microbial Threats in the Arctic: Proceedings of a Workshop Lauren Everett, Rapporteur Polar Research Board Board on Life Sciences Division on Earth and Life Studies Board on Global Health Health and Medicine Division In collaboration with the InterAcademy Partnership and the European Academies Science Advisory Council Copyright National Academy of Sciences. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Assistance to Researchers in Achieving High-Quality Broader Impacts
Assistance to Researchers in Achieving High-quality Broader Impacts 2011 COSEE Decadal Review Table of Contents COSEE California............................................................................................................................... 6 COSEE West......................................................................................................................................12 COSEE Central Gulf of Mexico......................................................................................................17 COSEE Florida (2002) ...................................................................................................................46 COSEE Southeast.............................................................................................................................52 COSEE Ocean Learning Communities .......................................................................................55 COSEE Great Lakes.........................................................................................................................70 COSEE Ocean Systems...................................................................................................................74 COSEE Alaska...................................................................................................................................77 COSEE Pacific Partnerships.........................................................................................................88 COSEE Coastal Trends...................................................................................................................95 -
Causes of Sea Level Rise
FACT SHEET Causes of Sea OUR COASTAL COMMUNITIES AT RISK Level Rise What the Science Tells Us HIGHLIGHTS From the rocky shoreline of Maine to the busy trading port of New Orleans, from Roughly a third of the nation’s population historic Golden Gate Park in San Francisco to the golden sands of Miami Beach, lives in coastal counties. Several million our coasts are an integral part of American life. Where the sea meets land sit some of our most densely populated cities, most popular tourist destinations, bountiful of those live at elevations that could be fisheries, unique natural landscapes, strategic military bases, financial centers, and flooded by rising seas this century, scientific beaches and boardwalks where memories are created. Yet many of these iconic projections show. These cities and towns— places face a growing risk from sea level rise. home to tourist destinations, fisheries, Global sea level is rising—and at an accelerating rate—largely in response to natural landscapes, military bases, financial global warming. The global average rise has been about eight inches since the centers, and beaches and boardwalks— Industrial Revolution. However, many U.S. cities have seen much higher increases in sea level (NOAA 2012a; NOAA 2012b). Portions of the East and Gulf coasts face a growing risk from sea level rise. have faced some of the world’s fastest rates of sea level rise (NOAA 2012b). These trends have contributed to loss of life, billions of dollars in damage to coastal The choices we make today are critical property and infrastructure, massive taxpayer funding for recovery and rebuild- to protecting coastal communities. -
Cumulative CO2 , PPM, and Temperature
Ocean-based Climate Solutions, Inc. www.ocean-based.com Santa Fe, NM 87501 505-231-7508 [email protected] All-Natural Biogeochemical CO2 Sequestration In Deep Ocean. Summary of Scientific Findings. Pump Design. Upwelling modeling, testing, data, and efficiency. Upwelling/Downwelling Estimated Annual Volumes. Downwelling Mechanics and Efficiencies. Nutrient Conversion and Net Carbon Sequestration From Upwelling. Dissolved Organic Carbon. Optimization: Projected Net CO2 Sequestered For Different Pumping Depths. Microbial Carbon Pump and Redfield Ratio. Safety Strategy. Environmental risk. CO2 Sequestration Estimate, Data Acquisition and Verification. Long-term Impact on Cumulative CO2 and Temperature Rise. Phased Installation and Cost Per Ton. Conclusion. References. Summary of Scientific Findings. • “…a new study from Woods Hole Oceanographic Institution (WHOI) shows that the efficiency of the ocean's "biological carbon pump" has been drastically underestimated, with implications for future climate assessments. By taking account of the depth of the euphotic, or sunlit zone, the authors found that about twice as much carbon sinks into the ocean per year than previously estimated.” [1] • Mathematical analysis and fluid dynamic modeling concludes that upwelled deep water quickly mixes and remains in the sunlit zone above the thermocline where the nutrients accumulate to trigger a bloom. [2] • Modeling also demonstrates when the warm, salty surface water is pumped down the tube, it cools and becomes denser below 300m, then sinking by gravity as it mixes into the deeper ocean. [3] • Deep water contains more nutrients as well as higher levels of dissolved CO2 compared to the surface ocean. Water upwelled from below about 300m contains surplus phosphate, enabling a second phytoplankton bloom that absorbs more CO2 than originally contained in the upwelled seawater. -
OCEAN WARMING • the Ocean Absorbs Most of the Excess Heat from Greenhouse Gas Emissions, Leading to Rising Ocean Temperatures
NOVEMBER 2017 OCEAN WARMING • The ocean absorbs most of the excess heat from greenhouse gas emissions, leading to rising ocean temperatures. • Increasing ocean temperatures affect marine species and ecosystems. Rising temperatures cause coral bleaching and the loss of breeding grounds for marine fishes and mammals. • Rising ocean temperatures also affect the benefits humans derive from the ocean – threatening food security, increasing the prevalence of diseases and causing more extreme weather events and the loss of coastal protection. • Achieving the mitigation targets set by the Paris Agreement on climate change and limiting the global average temperature increase to well below 2°C above pre-industrial levels is crucial to prevent the massive, irreversible impacts of ocean warming on marine ecosystems and their services. • Establishing marine protected areas and putting in place adaptive measures, such as precautionary catch limits to prevent overfishing, can protect ocean ecosystems and shield humans from the effects of ocean warming. The distribution of excess heat in the ocean is not What is the issue? uniform, with the greatest ocean warming occurring in The ocean absorbs vast quantities of heat as a result the Southern Hemisphere and contributing to the of increased concentrations of greenhouse gases in subsurface melting of Antarctic ice shelves. the atmosphere, mainly from fossil fuel consumption. The Fifth Assessment Report published by the Intergovernmental Panel on Climate Change (IPCC) in 2013 revealed that the ocean had absorbed more than 93% of the excess heat from greenhouse gas emissions since the 1970s. This is causing ocean temperatures to rise. Data from the US National Oceanic and Atmospheric Administration (NOAA) shows that the average global sea surface temperature – the temperature of the upper few metres of the ocean – has increased by approximately 0.13°C per decade over the past 100 years. -
Importance of Argo in Mediterranean Operational Oceanography Network (MOON)
Importance of Argo in Mediterranean Operational Oceanography Network (MOON) Srdjan Dobricic Centro Euro-Mediterraneo per i Cambiamenti Climatici and Nadia Pinardi Istituto Nazionale di Geofisica e Vulcanologia Italy OutlineOutline • The Operational Oceanographic Service in the Mediterranean Sea: products, core services and applications (downstream services) • Use of Argo floats in MOON TheThe OperationalOperational OceanographyOceanography approachapproach Numerical Multidisciplinary Data assimilation models of Multi-platform for optimal field hydrodynamics Observing estimates and ecosystem, system and coupled (permanent uncertainty a/synchronously and estimates relocatable) to atmospheric forecast Continuos production of nowcasts/forecasts of relevant environmental state variables The operational approach: from large to coastal space scales (NESTING), weekly to monthly time scales EuropeanEuropean OPERATIONALOPERATIONAL OCEANOGRAPHY:OCEANOGRAPHY: thethe GlobalGlobal MonitoringMonitoring ofof EnvironmentEnvironment andand SecuritySecurity (GMES)(GMES) conceptconcept The Marine Core Service will deliver regular and systematic reference information on the state of the oceans and regional seas of known quality and accuracy TheThe implementationimplementation ofof operationaloperational oceanographyoceanography inin thethe MediterraneanMediterranean Sea:Sea: 1995-today1995-today Numerical models of RT Observing System hydrodynamics satellite SST, SLA, and VOS-XBT, moored biochemistry multiparametric buoys, at basin scale ARGO and gliders -
Rapid and Significant Sea-Level Rise Expected If Global Warming Exceeds 2 °C, with Global Variation
Rapid and significant sea-level rise expected if global warming exceeds 2 °C, with global variation 06 April 2017 Issue 486 The world could experience the highest ever global sea-level rise in the Subscribe to free history of human civilisation if global temperature rises exceed 2 °C, predicts weekly News Alert a new study. Under current carbon-emission rates, this temperature rise will occur around the middle of this century, with damaging effects on coastal businesses and Source: Jevrejeva, S., ecosystems, while also triggering major human migration from low-lying areas. Global Jackson, L.P., Riva, R.E.M., sea-level rise will not be uniform, and will differ for different points of the globe. Grinsted, A. and Moore, J.C. (2016). Coastal sea level Sea-level rise is one of the biggest hazards of climate change. It threatens coastal rise with warming above populations, economic activity in maritime cities and fragile ecosystems. Because sea-level 2 °C. Proceedings of the rise is a delayed and complex response to past temperatures, sea levels will continue to National Academy of climb for centuries into the future, even after concentrations of greenhouse gases in the Sciences, 113(47): 13342– atmosphere have been stabilised. 13347. DOI: 10.1073/pnas.1605312113. This study, partly conducted under the EU RISES-AM project1, projected sea-level rise Contact: around the world under global warming of 2 °C (widely considered to be the threshold for [email protected] or john.m dangerous climate change), 4 °C, and 5 °C, compared with pre-industrial temperatures. This [email protected] was achieved by combining the results of 5 000 simulations of future sea level at each point on the globe, using 33 different climate models. -
A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods
water Review A Review of Ocean/Sea Subsurface Water Temperature Studies from Remote Sensing and Non-Remote Sensing Methods Elahe Akbari 1,2, Seyed Kazem Alavipanah 1,*, Mehrdad Jeihouni 1, Mohammad Hajeb 1,3, Dagmar Haase 4,5 and Sadroddin Alavipanah 4 1 Department of Remote Sensing and GIS, Faculty of Geography, University of Tehran, Tehran 1417853933, Iran; [email protected] (E.A.); [email protected] (M.J.); [email protected] (M.H.) 2 Department of Climatology and Geomorphology, Faculty of Geography and Environmental Sciences, Hakim Sabzevari University, Sabzevar 9617976487, Iran 3 Department of Remote Sensing and GIS, Shahid Beheshti University, Tehran 1983963113, Iran 4 Department of Geography, Humboldt University of Berlin, Unter den Linden 6, 10099 Berlin, Germany; [email protected] (D.H.); [email protected] (S.A.) 5 Department of Computational Landscape Ecology, Helmholtz Centre for Environmental Research UFZ, 04318 Leipzig, Germany * Correspondence: [email protected]; Tel.: +98-21-6111-3536 Received: 3 October 2017; Accepted: 16 November 2017; Published: 14 December 2017 Abstract: Oceans/Seas are important components of Earth that are affected by global warming and climate change. Recent studies have indicated that the deeper oceans are responsible for climate variability by changing the Earth’s ecosystem; therefore, assessing them has become more important. Remote sensing can provide sea surface data at high spatial/temporal resolution and with large spatial coverage, which allows for remarkable discoveries in the ocean sciences. The deep layers of the ocean/sea, however, cannot be directly detected by satellite remote sensors. -
Analyses of Altimetry Errors Using Argo and GRACE Data
1 Analyses of altimetry errors using Argo and GRACE data 2 J.-F. Legeais1, P. Prandi1, S. Guinehut1 3 1 Collecte Localisation Satellites, Parc Technologique du canal, 8-10 rue Hermès, 31520 Ramonville 4 Saint-Agne, France 5 Correspondence to : J.-F. Legeais ([email protected]) 6 Abstract. 7 This study presents the evaluation of the performances of satellite altimeter missions by comparing the altimeter 8 sea surface heights with in-situ dynamic heights derived from vertical temperature and salinity profiles measured 9 by Argo floats. The two objectives of this approach are the detection of altimeter drift and the estimation of the 10 impact of new altimeter standards that requires an independent reference. This external assessment method 11 contributes to altimeter Cal/Val analyses that cover a wide range of activities. Among them, several examples 12 are given to illustrate the usefulness of this approach, separating the analyses of the long-term evolution of the 13 mean sea level and its variability, at global and regional scales and results obtained via relative and absolute 14 comparisons. The latter requires the use of the ocean mass contribution to the sea level derived from GRACE 15 measurements. Our analyses cover the estimation of the global mean sea level trend, the validation of multi- 16 missions altimeter products as well as the assessment of orbit solutions. 17 Even if this approach contributes to the altimeter quality assessment, the differences between two versions of 18 altimeter standards are getting smaller and smaller and it is thus more difficult to detect their impact. It is 19 therefore essential to characterize the errors of the method, which is illustrated with the results of sensitivity 20 analyses to different parameters.