Congressional Record—House H11325

Total Page:16

File Type:pdf, Size:1020Kb

Congressional Record—House H11325 October 14, 2009 CONGRESSIONAL RECORD — HOUSE H11325 years has ever been given as an exam- people that will celebrate Diwali this (4) works closely with the Government of ple of this one human being that, by Saturday; I certainly hope it will be a the Philippines to improve disaster mitiga- the way, the former Prime Minister, joyous occasion. tion techniques and compliance among all Winston Churchill, described him as a Ms. ROS-LEHTINEN. Mr. Speaker, I key sectors of their societies. ‘‘naked fakir,’’ in very derogatory yield back the balance of my time. The SPEAKER pro tempore. Pursu- terms, I suppose, in that respect be- The SPEAKER pro tempore. The ant to the rule, the gentleman from cause Mr. Winston Churchill believed question is on the motion offered by American Samoa (Mr. Faleomavega) that the British Empire should rule for the gentleman from American Samoa and the gentlewoman from Florida (Ms. another 1,000 years perhaps. (Mr. FALEOMAVAEGA) that the House ROS-LEHTINEN) each will control 20 But I must say that, yes, there is ab- suspend the rules and agree to the reso- minutes. solutely no question that the life and lution, H. Res. 603. The Chair recognizes the gentleman the legacy of this great man, Mahatma The question was taken; and (two- from American Samoa. Gandhi, literally transformed even the thirds being in the affirmative) the GENERAL LEAVE civil rights movement here in our own rules were suspended and the resolu- Mr. FALEOMAVAEGA. Mr. Speaker, country. And for good, I say, yes, abso- tion was agreed to. I ask unanimous consent that all Mem- A motion to reconsider was laid on lutely, influenced people like Rosa bers may have 5 legislative days to re- the table. Parks, and especially the great and the vise and extend their remarks and in- late Martin Luther King, Jr. for what f clude extraneous material on the reso- he has done to transform American So- EXPRESSING SYMPATHY FOR THE lution under consideration. ciety, making it better than what it CITIZENS OF THE PHILIPPINES The SPEAKER pro tempore. Is there was. DEALING WITH TROPICAL STORM objection to the request of the gen- I would like to quote to my col- KETSANA AND TYPHOON PARMA tleman from American Samoa? leagues what Albert Einstein said: ‘‘I There was no objection. believe Gandhi’s views were the most Mr. FALEOMAVAEGA. Mr. Speaker, I move to suspend the rules and agree Mr. FALEOMAVAEGA. Mr. Speaker, enlightened of all the political men in to the resolution (H. Res. 800) express- I rise in strong support of this resolu- our time.’’ tion and yield myself such time as I Mr. Speaker, I yield back the balance ing sympathy for the citizens of the Philippines dealing with Tropical may consume. of my time. Mr. Speaker, this resolution extends Ms. ROS-LEHTINEN. To close on our Storm Ketsana and Typhoon Parma, as amended. our profound sympathies and condo- side, Mr. Speaker, I would like to yield lences to the good people of the Phil- 4 minutes to the gentleman from Cali- The Clerk read the title of the resolu- tion. ippines for the terrible losses they suf- fornia (Mr. ROYCE), the ranking mem- The text of the resolution is as fol- fered as a result of Tropical Storm ber on the Subcommittee on Ter- lows: Ketsana and Typhoon Parma. I would rorism, Nonproliferation, and Trade. like to thank my good friend and col- Mr. ROYCE. Mr. Speaker, let me H. RES. 800 league, Representative JACKIE SPEIER thank the gentlelady from Florida. Whereas, on September 26, 2009, Tropical As cochairman of the Congressional Storm Ketsana made landfall on the Phil- from California, for her leadership in Caucus on India and Indian Americans, ippines with the heaviest rainfall in 40 years introducing this important legislation. I rise in support of House Resolution equivalent to a typical month of rain during On September 26, Typhoon Ketsana monsoon season; 603, recognizing the 140th anniversary brought the heaviest rainfall in 40 Whereas 80 percent of the capital, Manila, years, leaving 80 percent of Manila of the birth of Mahatma Gandhi. was submerged under water as a result; Today, we give special remembrance under water. The storm killed more Whereas at least 3,000,000 persons have than 330 people, left nearly 40 missing, to one of the most revered people of the been affected by Tropical Storm Ketsana; last century. Preaching nonviolence, Whereas more than 135,470 families or forced more than 135,000 families into Gandhi dedicated his life’s work to 686,000 persons have been forced into evacu- evacuation centers, and destroyed or helping others. As a leader in the In- ation centers; badly damaged nearly 40,000 houses. dian National Congress, Gandhi led Whereas the casualties, as of October 9, Eight days later, Typhoon Parma hit campaigns to ease poverty. He led the 2009, include at least 237 dead, 308 injured, the Philippines, causing further de- and 37 missing; struction in areas that were still satu- campaigns to expand women’s rights. Whereas more than 4,640 houses were dam- And of course he is remembered for his rated by the previous storm and result- aged or destroyed; ing in the loss of an additional 28 lives. efforts to build religious amity. Above Whereas Tropical Storm Ketsana has all else, however, Gandhi worked tire- caused at least $4,800,000,000 in damages; I certainly would like to express my lessly to free his nation and helped di- Whereas following the devastation caused deepest condolences and sympathies to rect India into a new era of democracy. by Tropical Storm Ketsana, Typhoon Parma the families who lost their loved ones His methods to do this included lead- hit land October 2, 2009, bringing with it in the storms and to those who were in- ership by example. It included his orga- more torrential rain causing further flood- jured and displaced from their homes. nizational ability. It also included ing, landslides, crop damaged, and killing at It is my sincere hope that the good peaceful civil disobedience as a tool least 193 more people; people of the Philippines will find Whereas the United States and the Phil- strength and solace knowing that the and his power to persuade by force of ippines have a unique and enduring relation- argument. These were the ways in ship that is based on shared history and com- world stands by them in these very try- which he motivated those not only in mitment to democratic principles, as well as ing times. his own nation, but around the world on strong economic ties; The United States and the Phil- to this cause. Whereas the historical and cultural links ippines continue to maintain close ties Having traveled to India during the between the Philippines and the United based upon historical relations, com- second round of voting during India’s States remain important; and mon interests, and shared values. The recent election, the largest democratic Whereas the Filipino American community Filipino American community is the display the world has ever seen, I is the second largest Asian-American group second largest Asian American group in the United States with a population of ap- would have to say that Gandhi himself proximately 3,100,000: Now, therefore, be it in the United States, and they make an would indeed have been proud of how Resolved, That the House of Representa- invaluable contribution to our own far his nation has come. Under his tives— country here in America. guidance, India has become a plural- (1) mourns the terrible loss of life caused This resolution reflects our steadfast istic democracy of many religions and by Tropical Storm Ketsana and Typhoon commitment to this relationship, as ethnic groups, I think probably as plu- Parma that occurred on September 26, 2009, well as our strong desire for a speedy ralistic as the United States. We are and October 1, 2009; recovery of our friends in the Phil- (2) expresses its deepest condolences to the ippines who are suffering from the here today to help keep the spirit of families of the many victims; Gandhi alive and to remember his re- (3) urges President Obama to continue to aftermaths of these two major natural markable achievements. support the Philippines with emergency re- disasters. Before I close, I would also like to ex- lief supplies, logistical, transportation as- Mr. Speaker, I reserve the balance of tend my best wishes to the millions of sistance, and financial support; and my time. VerDate Nov 24 2008 00:31 Oct 15, 2009 Jkt 089060 PO 00000 Frm 00025 Fmt 7634 Sfmt 0634 E:\CR\FM\K14OC7.045 H14OCPT1 wwoods2 on DSK1DXX6B1PROD with HOUSE H11326 CONGRESSIONAL RECORD — HOUSE October 14, 2009 Ms. ROS-LEHTINEN. Mr. Speaker, to resulting in at least 337 deaths, 308 in- The ties between the United States open the debate on our side of the aisle, jured, and 37 missing. Then, just one and the Philippines are among the I am so pleased to yield such time as he week later, as Filipinos labored around strongest we have with any Asian may consume to the gentleman from the clock on recovery efforts, Typhoon country. Our two peoples have stood California (Mr. ROYCE), the ranking Parma struck Luzon, the heart of the together in war and in peace, with Fili- member on the Subcommittee on Ter- Philippine agricultural region which pino comrades-in-arms enduring, with rorism, Nonproliferation, and Trade. supplies half of the nation’s supply of our own veterans, the siege of Cor- Mr. ROYCE. I thank the gentlelady rice.
Recommended publications
  • Risk Reduction and Management in Escalating Water Hazards: How Fare the Poor?
    Risk Reduction and Management in Escalating Water Hazards: How Fare the Poor? Leonardo Q. Liongson, PhD The article aims to take stock of and rapidly assess the human and economic damages brought about, not only by Typhoon Yolanda, but also by the recent Bohol 7.2 magnitude earthquake and its aftershocks during the period October-November 2013, and comparatively, the most recent typhoons and monsoons (habagat) rainstorm and flood events in the 21st century. It will also cover the positive new steps and efforts of the infrastructure and S&T arms of the national government, and the needed additional steps and tasks which must follow, for alleviating and mitigating the hazard risks of water-based natural disasters, with emphasis on helping and protecting the most exposed and vulnerable to the hazard risks, being the poor sector of the society. The article has emphasized the need for implementing structural mitigation measures in poor unprotected towns and regions in the country, especially under the challenge and threat posed by growing population and climate change. Likewise, non-structural mitigation measures (which have shorter gestation periods of months and few years only, compared to decades for major structural measures) must be provided under the imperative or necessity implied by the structural gap of existing structures to adequately reduce and effectively manage the increasing flood and storm surge hazard risks, caused by growing population and climate change. NO PRIOR WARNING OF SUPER STORM SURGES of 225 kilometers per hour (kph) and gusts of 260 kph coming from PAGASA, with the attendant rains and the Many days before the first landfall of super Typhoon wind-blown piled-up sea waves hitting the coastal areas Haiyan (Yolanda) in Samar and Leyte (in Region 8) last of the region.
    [Show full text]
  • 6 2. Annual Summaries of the Climate System in 2009 2.1 Climate In
    2. Annual summaries of the climate system in above normal in Okinawa/Amami because hot and 2009 sunny weather was dominant under the subtropical high in July and August. 2.1 Climate in Japan (d) Autumn (September – November 2009, Fig. 2.1.1 Average surface temperature, precipitation 2.1.4d) amounts and sunshine durations Seasonal mean temperatures were near normal in The annual anomaly of the average surface northern and Eastern Japan, although temperatures temperature over Japan (averaged over 17 observatories swung widely. In Okinawa/Amami, seasonal mean confirmed as being relatively unaffected by temperatures were significantly above normal due to urbanization) in 2009 was 0.56°C above normal (based the hot weather in the first half of autumn. Monthly on the 1971 – 2000 average), and was the seventh precipitation amounts were significantly below normal highest since 1898. On a longer time scale, average nationwide in September due to dominant anticyclones. surface temperatures have been rising at a rate of about In contrast, in November, they were significantly 1.13°C per century since 1898 (Fig. 2.1.1). above normal in Western Japan under the influence of the frequent passage of cyclones and fronts around 2.1.2 Seasonal features Japan. In October, Typhoon Melor (0918) made (a) Winter (December 2008 – February 2009, Fig. landfall on mainland Japan, bringing heavy rainfall and 2.1.4a) strong winds. Since the winter monsoon was much weaker than (e) December 2009 usual, seasonal mean temperatures were above normal In the first half of December, temperatures were nationwide. In particular, they were significantly high above normal nationwide, and heavy precipitation was in Northern Japan, Eastern Japan and Okinawa/Amami.
    [Show full text]
  • Appendix 8: Damages Caused by Natural Disasters
    Building Disaster and Climate Resilient Cities in ASEAN Draft Finnal Report APPENDIX 8: DAMAGES CAUSED BY NATURAL DISASTERS A8.1 Flood & Typhoon Table A8.1.1 Record of Flood & Typhoon (Cambodia) Place Date Damage Cambodia Flood Aug 1999 The flash floods, triggered by torrential rains during the first week of August, caused significant damage in the provinces of Sihanoukville, Koh Kong and Kam Pot. As of 10 August, four people were killed, some 8,000 people were left homeless, and 200 meters of railroads were washed away. More than 12,000 hectares of rice paddies were flooded in Kam Pot province alone. Floods Nov 1999 Continued torrential rains during October and early November caused flash floods and affected five southern provinces: Takeo, Kandal, Kampong Speu, Phnom Penh Municipality and Pursat. The report indicates that the floods affected 21,334 families and around 9,900 ha of rice field. IFRC's situation report dated 9 November stated that 3,561 houses are damaged/destroyed. So far, there has been no report of casualties. Flood Aug 2000 The second floods has caused serious damages on provinces in the North, the East and the South, especially in Takeo Province. Three provinces along Mekong River (Stung Treng, Kratie and Kompong Cham) and Municipality of Phnom Penh have declared the state of emergency. 121,000 families have been affected, more than 170 people were killed, and some $10 million in rice crops has been destroyed. Immediate needs include food, shelter, and the repair or replacement of homes, household items, and sanitation facilities as water levels in the Delta continue to fall.
    [Show full text]
  • Two Phytoplankton Blooms Near Luzon Strait Generated by Lingering Typhoon Parma
    Two phytoplankton blooms near Luzon Strait generated by Lingering Typhoon Parma Hui Zhao1, Guoqi Han2, Shuwen Zhang1, and Dongxiao Wang3 1College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China 2 Northwest Atlantic Fisheries Centre, Fisheries and Oceans Canada, St. John’s, NL, Canada 3. State Key Laboratory of Tropical Oceanography(LTO),SCSIO, CAS Introduction A. WS,EKV, Sep 15-30, 2009 B. WS, EKV, OCT 4-5, 2009 Typhoons or tropical cyclones occur frequently in the South China Sea (SCS), over 7 times 22N annually on average. Due to limit of nutrients, cyclones and typhoons have important effects on chlorophyll-a (Chl-a) and phytoplankton blooms in oligotrophic ocean waters of the SCS. 20N Typhoons in the region, with different translation speeds and intensities, exert diverse impacts on intensity and area of phytoplankton blooms. However, role of longer-lingering weak cyclones 18N played phytoplankton biomass was seldom investigated in SCS. Parma was one slow-moving and relatively weak (≤Ca. 1), while lingering near the 16N northern Luzon Island for about 7 days in an area of 3°by 3°(Fig. 1). This kind of long lingering typhoons are rather infrequent in the SCS, and their influences on phytoplankton 118E 120E122E 124E 118E 120E122E 124E Fig. 2 Surface Wind Vectors (m s-1 , respectively) and Ekman Pumping blooms have seldom been evaluated. In this work, we investigate two phytoplankton blooms Velocity (EPV) (color shaded in 10-4 m s-1). (A) Before Typhoon; (B). During (one offshore and the other nearshore) north of Luzon Island and the impacts of typhoon’s Fig 1 Track and intensity of Typhoon Parma (2009) in the Study area.
    [Show full text]
  • Potential Impact of Climate Change and Extreme Events on Slope Land Hazard
    Potential Impact of Climate Change and Extreme Events on Slope Land Hazard - A Case Study of Xindian Watershed in Taiwan Shih-Chao WEI1, Hsin-Chi LI2, Hung-Ju SHIH2, Ko-Fei LIU1 1 Department of Civil Engineering, National Taiwan University, Taipei 10617, Taiwan 5 2 National Science and Technology Center for Disaster Reduction, New Taipei City 23143, Taiwan Correspondence to: Hsin-Chi LI ([email protected]) Abstract. The production and transportation of sediment in mountainous areas caused by extreme rainfall events triggered by climate change is a challenging problem, especially in watersheds. To investigate this issue, the present study adopted the scenario approach coupled with simulations using various models. Upon careful model selection, the simulation of projected 10 rainfall, landslide, debris flow, and loss assessment were integrated by connecting the models’ input and output. The Xindian watershed upstream from Taipei, Taiwan, was identified and two extreme rainfall scenarios from the late 20th and 21st centuries were selected to compare the effects of climate change. Using sequence simulations, the chain reaction and compounded disaster were analysed. Moreover, the potential effects of slope land hazards were compared between the present and future, and the likely impacts in the selected watershed areas were discussed with respect to extreme climate. The results 15 established that the unstable sediment volume would increase by 28.81% in terms of the projected extreme event. The total economic losses caused by the chain impacts of slope land disasters under climate change would be increased to US$ 358.25 million. Owing to the geographical environment of the Taipei metropolitan area, the indirect losses of water supply shortage caused by slope land disasters would be more serious than direct losses.
    [Show full text]
  • Disaster Response Shelter Catalogue
    Disaster Response Shelter Catalogue Disaster Response Shelter Catalogue Disaster Response Shelter Catalogue Copyright 2012 Habitat for Humanity International Front cover: Acknowledgements Sondy-Jonata Orientus’ family home was destroyed in the 2010 earthquake We are extremely grateful to all the members of the Habitat for Humanity that devastated Haiti, and they were forced to live in a makeshift tent made of network who made this publication possible. Special thanks to the global tarpaulins. Habitat for Humanity completed the family’s new home in 2011. © Habitat Disaster Response community of practice members. Habitat for Humanity International/Ezra Millstein Compilation coordinated by Mario C. Flores Back cover: Editorial support by Phil Kloer Top: Earthquake destruction in Port-au-Prince, Haiti. © Habitat for Humanity International Steffan Hacker Contributions submitted by Giovanni Taylor-Peace, Mike Meaney, Ana Cristina Middle: Reconstruction in Cagayan de Oro, Philippines, after tropical storm Washi. Pérez, Pete North, Kristin Wright, Erwin Garzona, Nicolas Biswas, Jaime Mok, © Habitat for Humanity Internationa/Leonilo Escalada Scarlett Lizana Fernández, Irvin Adonis, Jessica Houghton, V. Samuel Peter, Bottom: A tsunami-affected family in Indonesia in front of their nearly completed Justin Jebakumar, Joseph Mathai, Andreas Hapsoro, Rudi Nadapdap, Rashmi house. © Habitat for Humanity International/Kim McDonald Manandhar, Amrit Bahadur B.K., Leonilo (Tots) Escalada, David (Dabs) Liban, Mihai Grigorean, Edward Fernando, Behruz Dadovoeb, Kittipich Musica, Additional photo credits: Ezra Millstein, Steffan Hacker, Jaime Mok, Mike Meaney, Nguyen Thi Yen. Mario Flores, Kevin Kehus, Maria Chomyszak, Leonilo (Tots) Escalada, Mikel Flamm, Irvin Adonis, V. Samuel Peter, Sara E. Coppler, Tom Rogers, Joseph Mathai, Additional thanks to Heron Holloway and James Samuel for reviewing part of Justin Jebakumar, Behruz Dadovoeb, Gerardo Soto, Mihai Gregorian, Edward the materials.
    [Show full text]
  • The Change in Rainfall from Tropical Cyclones Due to Orographic Effect of the Sierra Madre Mountain Range in Luzon, Philippines
    Philippine Journal of Science 145 (4): 313-326, December 2016 ISSN 0031 - 7683 Date Received: ?? Feb 20?? The Change in Rainfall from Tropical Cyclones Due to Orographic Effect of the Sierra Madre Mountain Range in Luzon, Philippines Bernard Alan B. Racoma1,2*, Carlos Primo C. David1, Irene A. Crisologo1, and Gerry Bagtasa3 1National Institute of Geological Sciences, College of Science, University of the Philippines, Diliman, Quezon City, Philippines 2Nationwide Operational Assessment of Hazards, University of the Philippines, Diliman, Quezon City, Philippines 3Institute of Environmental Science and Meteorology, College of Science, University of the Philippines, Diliman, Quezon City, Philippines This paper discusses the Sierra Madre Mountain Range of the Philippines and its associated influence on the intensity and distribution of rainfall during tropical cyclones. Based on Weather and Research Forecasting model simulations, a shift in rainfall was observed in different portions of the country, due to the reduction of the topography of the mountain. Besides increasing the rainfall along the mountain range, a shift in precipitation was observed during Tropical Storm Ondoy, Typhoon Labuyo, and Tropical Storm Mario. It was also observed that the presence of the Sierra Madre Mountain Range slows down the movement of a tropical cyclones, and as such allowing more time for precipitation to form over the country. Wind profiles also suggest that the windward and leeward sides of mountain ranges during Tropical Cyclones changes depending on the storm path. It has been suggested that in predicting the distribution of rainfall, the direction of movement of a tropical cyclones as well as its adjacent areas be taken into great consideration.
    [Show full text]
  • (May 2008 to April 2010): Climate Variability and Weather Highlights
    1 2 The "Year" of Tropical Convection (May 2008 to April 2010): 3 Climate Variability and Weather Highlights 4 5 6 7 Duane E. Waliser1, Mitch Moncrieff2, David Burrridge3, Andreas H. Fink4, Dave Gochis2, 8 B. N. Goswami2, Bin Guan1, Patrick Harr6, Julian Heming7, Huang-Hsuing Hsu8, Christian 9 Jakob9, Matt Janiga10, Richard Johnson11, Sarah Jones12, Peter Knippertz13, Jose Marengo14, 10 Hanh Nguyen10, Mick Pope9, Yolande Serra15, Chris Thorncroft10, Matthew Wheeler16, 11 Robert Wood17, Sandra Yuter18 12 13 1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA 14 2National Center for Atmospheric Research, Boulder, CO, USA 15 3THORPEX International Programme Office, World Meteorological Office, Geneva, Switzerland 16 4der Universitaet zu Koeln, Koeln, Germany 17 5Indian Institute of Tropical Meteorology, Pune, India 18 6Naval Postgraduate School, Monterey, CA, USA 19 7United Kingdom Meteorological Office, Exeter, England 20 8National Taiwan University, Taipei, Taiwan 21 9Melbourne University, Melbourne, Australia 22 10State University of New York, Albany, NY, USA 23 11Colorado State University, Fort Collins, CO, USA 24 12 Karlsruhe Institute of Technology, Karlsruhe, Germany 25 13University of Leeds, Leeds, England 26 14Centro de Previsão de Tempo e Estudos Climáticos, Sao Paulo, Brazil 27 15University of Arizona, Tucson, AZ, USA 28 16Centre for Australian Weather and Climate Research, Melbourne, Australia 29 17University of Washington, Seattle, USA 30 18North Caroline State University, Raleigh, NC, USA 31 32 33 34 Submitted to the 35 Bulletin of the American Meteorological Society 36 November 2010 37 38 Corresponding author: Duane Waliser, [email protected], Jet Propulsion Laboratory, MS 39 183-505, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109 40 1 1 Abstract 2 The representation of tropical convection remains a serious challenge to the skillfulness of our 3 weather and climate prediction systems.
    [Show full text]
  • Fifth Storm in Three Weeks Leaves Filipinos Trapped in Houses, on Roofs
    Fifth storm in three weeks leaves Filipinos trapped in houses, on roofs MANILA, Philippines (CNS) — Filipinos appealed for help as a fifth tropical storm or typhoon hit their country in a three- week period. These included the strongest typhoon since 2013 and the biggest floods since 2009. The latest, Typhoon Vamco — or Ulysses as it is known in Philippines — left at least 42 dead and 20 missing. Rescue workers said Nov. 13 they were still trying to reach people trapped in their houses, even after the storm blew out to sea. In eastern metropolitan Manila, water in the Marikina River rose to 72 feet, surpassing Typhoon Ketsana, which left 671 dead in 2009, the United Nations reported. Ucanews.com said Jesuits in the Philippines have appealed for material and spiritual support for victims of Vamco; many residents in Marikina City took refuge on the rooftops of their homes to await rescue. Ucanews.com reported Typhoon Vamco also brought misery to other areas still trying to recover from Super Typhoon Goni, which struck Nov. 1. That typhoon was the strongest since Haiyan, which hit in 2013. Aid agencies such as Caritas and its U.S. partner, Catholic Relief Services, were already helping people from Goni. Agencies said the main needs were for food, shelter, health assistance and mental health and psychosocial support. Marikina City Mayor Marcelino Teodoro also issued an appeal for help, reported ucanews.com. “Local authorities in Marikina City cannot conduct rescue efforts alone. Given the weather, we need air support. People are on their rooftops waiting to be rescued,” Teodoro told reporters.
    [Show full text]
  • Geohazards, Tropical Cyclones and Disaster Ris Management
    Journal of Environmental Science and Management 16(1) : 84-97 (June 2013) ISSN 0119-1144 *2 Climate change, involving both natural climate variability and anthropogenic global warming, has been a major worldwide concern, particularly with the publication of the Fourth Assessment Report (AR4) of the Intergovernmental Panel on Climate Change. Considering the archipelagic nature of the Philippines and its being a very minor emitter of greenhouse gases, adaptation to climate change has been the Government’s national policy. The importance of expediting these climate change-related adaptation measures was highlighted by a string of geo-meteorological- 2009. We present the geologic conditions that rendered the affected areas, especially in northwestern Luzon, extremely vulnerable to the existent hazards, the meteorological conditions that set off the disaster and the different initiatives that the government and local communities have taken to further prepare the people for possible future disasters. Recognition of the pertinent issues and the extant challenges points to the urgent need for mainstreaming both geo-meteorological- related disaster risk management and climate change adaptation measures in the light of changing climate conditions. climate change adaptation, disaster risk management, geo-meteorological hazards, tropical cyclone, Luzon, Philippines Asian Development Bank (ADB) 2009Lagmay et al. 2006 Yumul et al. 2006
    [Show full text]
  • 2009 Typhoon Ondoy and Pepeng Disasters in the Phillipines
    Natural Disaster Research Report of the National Research Institute for Earth Science and Disaster Prevention, No. 45 ; February, 2011 2009 Typhoon Ondoy and Pepeng Disasters in the Phillipines Tadashi NAKASU*, Teruko SATO**, Takashi INOKUCHI***, Shinya SHIMOKAWA***, and Akiko WATANABE**** * International Centre for Water Hazard and Risk Management under the auspices of UNESCO (ICHARM), Japan ** Visiting Researcher, National Research Institute for Earth Science and Disaster Prevention (NIED), Japan, *** National Research Institute for Earth Science and Disaster Prevention (NIED), Japan **** Toyo University, Japan Abstract On September 25 and 26, 2009, Typhoon Ondoy struck the south-west island of the Luzon islands in the Philippines. Heavy rainfall affected 4.9 million people, causing 501 fatalities. In the middle of October 2009, Typhoon Pepeng struck in and around Baguio City, located in the northern part of the Luzon islands. Heavy rainfall caused a large number of landslides, and 4.5 million people were affected, totaling 539 fatalities. This is a survey report of the great water related disasters that occurred in the Philippines and that were caused by Typhoons Ondoy and Pepeng. The report is focused on the extensive urban flood disaster that occurred in Metro Manila and on the landslides that occurred in and around Baguio City. The investigation was managed and carried out by an interdisciplinary team including a geologist, a geophysical scientist, a geographer, a sociologist, and an anthropologist. This research reveals that changes in socio-economic conditions increases vulnerability to disasters and thereby exacerbates damage. It is suggested that future rapid population growth in urban areas along with global warming could further increase vulnerability to disasters in developing countries.
    [Show full text]
  • Statistical Characteristics of the Response of Sea Surface Temperatures to Westward Typhoons in the South China Sea
    remote sensing Article Statistical Characteristics of the Response of Sea Surface Temperatures to Westward Typhoons in the South China Sea Zhaoyue Ma 1, Yuanzhi Zhang 1,2,*, Renhao Wu 3 and Rong Na 4 1 School of Marine Science, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] 2 Institute of Asia-Pacific Studies, Faculty of Social Sciences, Chinese University of Hong Kong, Hong Kong 999777, China 3 School of Atmospheric Sciences, Sun Yat-Sen University and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China; [email protected] 4 College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao 266100, China; [email protected] * Correspondence: [email protected]; Tel.: +86-1888-885-3470 Abstract: The strong interaction between a typhoon and ocean air is one of the most important forms of typhoon and sea air interaction. In this paper, the daily mean sea surface temperature (SST) data of Advanced Microwave Scanning Radiometer for Earth Observation System (EOS) (AMSR-E) are used to analyze the reduction in SST caused by 30 westward typhoons from 1998 to 2018. The findings reveal that 20 typhoons exerted obvious SST cooling areas. Moreover, 97.5% of the cooling locations appeared near and on the right side of the path, while only one appeared on the left side of the path. The decrease in SST generally lasted 6–7 days. Over time, the cooling center continued to diffuse, and the SST gradually rose. The slope of the recovery curve was concentrated between 0.1 and 0.5.
    [Show full text]