Earth Observations for Environmental Sustainability for the Next Decade
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World Risk Report 2012
Focus: Environmental degradation and disasters WorldRiskReport 2012 In cooperation with UNU-EHS Institute for Environment and Human Security Together for people in need. WorldRiskReport 2012 1. Disaster risk, environmental degradation and global sustainability policy ................ 5 Peter Mucke 2. WorldRiskIndex 2012: Concept, updating and results ................................ 11 Torsten Welle, Jörn Birkmann, Jakob Rhyner, Maximilian Witting, Jan Wolfertz 2.1 Concept and structure of the WorldRiskIndex .................................... 12 2.2 Updating and modifying the indicators ......................................... 16 2.3 Risk assessment at global level for 2012 ........................................ 18 3. Focus: Environmental degradation and disasters .................................... 27 3.1 Environmental degradation as a risk factor ...................................... 28 Torsten Welle, Michael W. Beck, Peter Mucke 3.2 Coastal Habitats and Risk Reduction ........................................... 32 Michael W. Beck, Christine C. Shepard 3.3 Agrofuels, land-grabbing and landslides ....................................... 42 Katja Maurer 3.4 Environmental degradation, poverty and disaster risk on the international development agenda ...................................... 48 Jens Martens 4. Disaster risk reduction – a key element of global sustainability policy ................... 57 Peter Mucke, Jens Martens, Katrin Radtke Annex ........................................................................... 63 WorldRiskReport -
Friday) Time • 7.30 P.M
Date • 21st February 2014 (Friday) Time • 7.30 p.m. to 10.00 p.m. Venue • Ballroom 1 & 2, 1st Floor Sime Darby Convention Centre 1A, Jalan Bukit Kiara 1, K. L. CoNTENTS OUR Journey , • Our Journey 3 In 1995 during the height of the Rwanda crisis, 2 American doctors, • Message from the Executive Director 4 Drs. Mark and Betsy Neuenschwander of the International Health Services Foundation received a vision from God to raise up disaster • Message from Drs. Mark & Betsy 5 relief teams across the world. They visited Malaysia and conducted • Vision & Mission 6 3 consecutive Disaster Relief Schools (DRS) in 1995, 1996 and 1997. From these training schools, a group of graduates received • Where We Have Served 7 - 10 God’s call to establish a disaster relief organization in Asia. • Reflections from the Journey 11 On 3rd December 1998, • The Joy of A Special Child by Cynthia, Volunteer 12 - 13 CREST was birthed in Malaysia. • I Am Blessed by Dr. Oh Swee Eng, Volunteer 14 - 15 • Walking By Faith by Martin Chow, Volunteer 16 -17 • Moving Beyond Emergency Response by Dr. Yoong Sao Chin, CREST Director 18 • Early Childhood Development Centre (ECDC) 19 • An Interview With Wong Lee Sin, Volunteer 20 - 21 • Out of the Classroom & Into the Field by Michelle Choo, Volunteer 22 - 23 • Once Is Not Enough by Susan Chen, Volunteer 24 - 25 • Aknowledgement 26 • Congratulatory & Advertisement 27 - 34 Now, CREST serves in countries across Asia and takes on the mantle to train more relief volunteers in Malaysia and beyond. CREST has also moved beyond mere active emergency response into rehabilitation and reconstruction with the ultimate goal of impacting communities into self dignity and reliance. -
4. the TROPICS—HJ Diamond and CJ Schreck, Eds
4. THE TROPICS—H. J. Diamond and C. J. Schreck, Eds. Pacific, South Indian, and Australian basins were a. Overview—H. J. Diamond and C. J. Schreck all particularly quiet, each having about half their The Tropics in 2017 were dominated by neutral median ACE. El Niño–Southern Oscillation (ENSO) condi- Three tropical cyclones (TCs) reached the Saffir– tions during most of the year, with the onset of Simpson scale category 5 intensity level—two in the La Niña conditions occurring during boreal autumn. North Atlantic and one in the western North Pacific Although the year began ENSO-neutral, it initially basins. This number was less than half of the eight featured cooler-than-average sea surface tempera- category 5 storms recorded in 2015 (Diamond and tures (SSTs) in the central and east-central equatorial Schreck 2016), and was one fewer than the four re- Pacific, along with lingering La Niña impacts in the corded in 2016 (Diamond and Schreck 2017). atmospheric circulation. These conditions followed The editors of this chapter would like to insert two the abrupt end of a weak and short-lived La Niña personal notes recognizing the passing of two giants during 2016, which lasted from the July–September in the field of tropical meteorology. season until late December. Charles J. Neumann passed away on 14 November Equatorial Pacific SST anomalies warmed con- 2017, at the age of 92. Upon graduation from MIT siderably during the first several months of 2017 in 1946, Charlie volunteered as a weather officer in and by late boreal spring and early summer, the the Navy’s first airborne typhoon reconnaissance anomalies were just shy of reaching El Niño thresh- unit in the Pacific. -
NASA Sees Typhoon Noru Raging Near the Minami Tori Shima Atoll 24 July 2017
NASA sees Typhoon Noru raging near the Minami Tori Shima Atoll 24 July 2017 north latitude and 154.9 degrees east longitude. That's about 128 nautical miles north of Minami Tori Shima. It was moving to the east-southeast at 13.8 mph (12 knots/22.2 kph). Noru is located to the southwest of Tropical Storm Koru, which is a much smaller and weaker storm. Noru is moving in a cyclonic loop and is forecast to turn back toward the west by July 26. The Joint Typhoon Warning Center's forecast calls for the storm to approach the island of Iwo To, Japan around July 29. Provided by NASA's Goddard Space Flight Center On July 24 at 0342 UTC (July 23 at 11:42 p.m. EDT) NASA-NOAA's Suomi NPP satellite captured a visible image of Typhoon Noru in the Northwestern Pacific Ocean. Credit: NASA/NOAA NASA-NOAA's Suomi NPP satellite captured an image of Typhoon Noru raging near the unpopulated atoll of Minami Tori Shima in the Northwestern Pacific Ocean. Minami-Tori-shima or Marcus Island is an isolated Japanese coral atoll about 1,150 miles (1,850 kilometers) southeast of Tokyo. On July 24 at 0342 UTC (July 23 at 11:42 p.m. EDT), the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite provided a visible-light image of Typhoon Noru. The VIIRS image showed a cloud-covered eye surrounded by a thick band of powerful thunderstorms and a thick band wrapping into the center from the southeastern quadrant. -
NASA Satellite Sees Typhoon Noru in Infrared Light 31 July 2017
NASA satellite sees Typhoon Noru in infrared light 31 July 2017 To Island, Japan. Maximum sustained winds were near 143.8 mph (125 knots/231 kph). Noru was moving to the west at 6.9 mph (6 knots/11.1 kph). The Joint Typhoon Warning Center forecasts Noru to move slowly to the northwest over the next several days and move toward Kyushu, Japan. Noru is expected to near Kyushu around August 5. Kyushu is the third biggest island of Japan and located farthest southwest of Japan's four main islands. Provided by NASA's Goddard Space Flight Center NASA-NOAA's Suomi NPP satellite captured this infrared image of Typhoon Noru on July 30, 2017, at 11:50 a.m. EDT (1550 UTC) in the Northwestern Pacific Ocean. Credit: University of Wisconsin- Madison/CIMSS/William Straka III NASA-NOAA's Suomi NPP satellite captured an infrared image of Typhoon Noru that showed the structure and cloud top temperatures of the powerful thunderstorms circling its eye. On July 27, 2017 at 12:24 a.m. EDT (0424 UTC) the Visible Infrared Imaging Radiometer Suite (VIIRS) instrument aboard NASA-NOAA's Suomi NPP satellite provided an infrared image of Typhoon Noru. The VIIRS image revealed very cold cloud top temperatures as cold as 190 Kelvin (minus 83.1 degrees Celsius/minus 117.7 degrees Fahrenheit) in thunderstorms circling the eye. Thunderstorms with cloud tops that high in the troposphere have been shown to generate heavy rain. At 11 a.m. EDT (1500 UTC) on July 30, the center of Typhoon Noru was located near 23.0 degrees north latitude and 139.3 degrees east longitude. -
Launching the International Decade for Natural Disaster Reduction
210 91NA ECONOMIC AND SOCIAL COMMISSION FOR ASIA AND THE PACIFIC BANGKOK, THAILAND NATURAL DISASTER REDUCTION IN ASIA AND THE PACIFIC: LAUNCHING THE INTERNATIONAL DECADE FOR NATURAL DISASTER REDUCTION VOLUME I WATER-RELATED NATURAL DISASTERS UNITED NATIONS December 1991 FLOOD CONTROL SERIES 1* FLOOD DAMAGE AND FLOOD CONTROL ACnVITlHS IN ASIA AND THE FAR EAST United Nations publication, Sales No. 1951.II.F.2, Price $US 1,50. Availably in separate English and French editions. 2* MKTUODS AND PROBLEMS OF FLOOD CONTROL IN ASIA AND THIS FAR EAST United Nations publication, Sales No, 1951.ILF.5, Price SUS 1.15. 3.* PROCEEDINGS OF THF. REGIONAL TECHNICAL CONFERENCE ON FLOOD CONTROL IN ASIA AND THE FAR EAST United Nations publication, Sales No. 1953.U.F.I. Price SUS 3.00. 4.* RIVER TRAINING AND BANK PROTECTION • United Nations publication, Sate No. 1953,TI.I;,6. Price SUS 0.80. Available in separate English and French editions : 1* THE SKDLMENT PROBLEM United Nations publication, Sales No. 1953.TI.F.7. Price $US 0.80. Available in separate English and French editions 6.* STANDARDS FOR METHODS AND RECORDS OF HYDROLOGIC MEASUREMENTS United Nations publication, Sales No. 1954.ILF.3. Price SUS 0.80. Available, in separate. English and French editions. 7.* MULTIPLE-PURPOSE RIVER DEVELOPMENT, PARTI, MANUAL OF RIVER BASIN PLANNING United Nations publication. Sales No. 1955.II.I'M. Price SUS 0.80. Available in separate English and French editions. 8.* MULTI-PURPOSE RIVER DEVELOPMENT, PART2A. WATER RESOURCES DEVELOPMENT IN CF.YLON, CHINA. TAIWAN, JAPAN AND THE PHILIPPINES |;_ United Nations publication, Sales No. -
Evaluations on Vortex Based Doppler Velocity Dealiasing Algorithm for Tropical Cyclones
Evaluations on Vortex Based Doppler Velocity Dealiasing Algorithm for Tropical Cyclones Wei-Tin Fang1, Pao-Liang Chang2, Pin-Fang Lin1 Meteorological Satellite Center1, Meteorological Information Center2 Central Weather Bureau, Taipei, Taiwan Abstract In this study, a vortex-based Doppler velocity dealiasing (VDVD) algorithm with iterative procedures based on the Rankine combined vortex assumption is proposed to improve Doppler velocity quality for tropical cyclone (TC) cases. An idealized case based on the ground-based velocity track display (GBVTD) and GBVTD-simplex techniques shows reasonable results for recovering the aliased velocity and finding the proper TC center. For Typhoon Fitow (2013), which was observed by Wu-Fen-San radar, the proposed vortex-based Doppler velocity dealiasing algorithm recovers most of the aliased velocity observations with 99.4 % accuracy for all pixels, based on 472 data sweeps. For 87 % (95.6 %) of data sweeps, the data success rate is more than 99 % (98 %), compared to that of 70.6 % (79.7 %) for data sweeps when using the Zhang and Wang (2006) (hereafter, ZW06) algorithm. In addition, there is a data success rate of approximately 2 % for sweeps lower than 97 % when using the VDVD algorithm, compared to that of more than 14 % of sweeps when using the ZW06 algorithm. The success rate of the VDVD for each sweep varies from 93.6 to 100 %, and the success rate of the ZW06 algorithm varies from 74.5 to 99.97 %. In addition, it is found that the local circulations generated by terrain would might conflict with the assumption of Rankine combined vortex and result in inadequate dealiased Doppler velocities from VDVD algorithm. -
NASA's Aqua Satellite Tracking Typhoon Noru in Northwestern Pacific 28 July 2017
NASA's Aqua satellite tracking Typhoon Noru in northwestern Pacific 28 July 2017 was moving toward the northwest near 9 knots (10.3 mph/16.6 kph). The JTWC noted that the intensity is forecast "to remain steady for the next 24 hours as dry air and moderate vertical wind shear are offset by higher sea surface temperatures and the development of an equatorward outflow channel. Beyond one day, Noru is forecast to intensify as it tracks over increasingly warm sea surface temperatures and a point source develops over top of the system." In addition to Noru, there's another typhoon in the Northwestern Pacific Ocean that lies to the west of Noru. Typhoon Nesat is headed for a landfall in On July 27 NASA's Aqua satellite captured a visible Taiwan on July 29. image of Typhoon Noru in the Northwestern Pacific Ocean. Credit: NASA Goddard MODIS Rapid Response Despite Noru's distance from Taiwan, the Taiwan Team Central Weather Bureau is also tracking the storm. For updated forecasts, visit: http://www.cwb.gov.tw/V7e/. NASA's Aqua satellite passed over Typhoon Noru in the Northwestern Pacific Ocean as the storm Provided by NASA's Goddard Space Flight Center continued moving toward the southwest and remaining far from the big island of Japan. On July 27 at 1:30 p.m. local time the Moderate Resolution Imaging Spectroradiometer or MODIS instrument aboard NASA's Aqua satellite captured a visible image of the storm that showed some powerful thunderstorms surrounding the center of circulation. The Joint Typhoon Warning Center (JTWC) noted on July 28, "animated multispectral satellite imagery depicts a struggling system with limited convection." On July 28 at 5 a.m. -
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. -
Objective Estimation of Tropical Cyclone Intensity from Active and Passive Microwave Remote Sensing Observations in the Northwestern Pacific Ocean
remote sensing Article Objective Estimation of Tropical Cyclone Intensity from Active and Passive Microwave Remote Sensing Observations in the Northwestern Pacific Ocean Kunsheng Xiang 1,2,3, Xiaofeng Yang 1,3,* , Miao Zhang 4, Ziwei Li 1 and Fanping Kong 1,2 1 State Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth, Chinese Academy of Sciences, Beijing 100101, China; [email protected] (K.X.); [email protected] (Z.L.); [email protected] (F.K.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 The Hainan Key Laboratory of Earth Observation, Sanya 572029, China 4 Key Lab of Radiometric Calibration and Validation for Environmental Satellites, China Meteorological Administration (LRCVES/CMA) and National Satellite Meteorological Center, Beijing 100081, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-64806215 Received: 18 February 2019; Accepted: 11 March 2019; Published: 14 March 2019 Abstract: A method of estimating tropical cyclone (TC) intensity based on Haiyang-2A (HY-2A) scatterometer, and Special Sensor Microwave Imager and Sounder (SSMIS) observations over the northwestern Pacific Ocean is presented in this paper. Totally, 119 TCs from the 2012 to 2017 typhoon seasons were selected, based on satellite-observed data and China Meteorological Administration (CMA) TC best track data. We investigated the relationship among the TC maximum-sustained wind (MSW), the microwave brightness temperature (TB), and the sea surface wind speed (SSW). Then, a TC intensity estimation model was developed, based on a multivariate linear regression using the training data of 96 TCs. Finally, the proposed method was validated using testing data from 23 other TCs, and its root mean square error (RMSE), mean absolute error (MAE), and bias were 5.94 m/s, 4.62 m/s, and −0.43 m/s, respectively. -
Capital Adequacy (E) Task Force RBC Proposal Form
Capital Adequacy (E) Task Force RBC Proposal Form [ ] Capital Adequacy (E) Task Force [ x ] Health RBC (E) Working Group [ ] Life RBC (E) Working Group [ ] Catastrophe Risk (E) Subgroup [ ] Investment RBC (E) Working Group [ ] SMI RBC (E) Subgroup [ ] C3 Phase II/ AG43 (E/A) Subgroup [ ] P/C RBC (E) Working Group [ ] Stress Testing (E) Subgroup DATE: 08/31/2020 FOR NAIC USE ONLY CONTACT PERSON: Crystal Brown Agenda Item # 2020-07-H TELEPHONE: 816-783-8146 Year 2021 EMAIL ADDRESS: [email protected] DISPOSITION [ x ] ADOPTED WG 10/29/20 & TF 11/19/20 ON BEHALF OF: Health RBC (E) Working Group [ ] REJECTED NAME: Steve Drutz [ ] DEFERRED TO TITLE: Chief Financial Analyst/Chair [ ] REFERRED TO OTHER NAIC GROUP AFFILIATION: WA Office of Insurance Commissioner [ ] EXPOSED ________________ ADDRESS: 5000 Capitol Blvd SE [ ] OTHER (SPECIFY) Tumwater, WA 98501 IDENTIFICATION OF SOURCE AND FORM(S)/INSTRUCTIONS TO BE CHANGED [ x ] Health RBC Blanks [ x ] Health RBC Instructions [ ] Other ___________________ [ ] Life and Fraternal RBC Blanks [ ] Life and Fraternal RBC Instructions [ ] Property/Casualty RBC Blanks [ ] Property/Casualty RBC Instructions DESCRIPTION OF CHANGE(S) Split the Bonds and Misc. Fixed Income Assets into separate pages (Page XR007 and XR008). REASON OR JUSTIFICATION FOR CHANGE ** Currently the Bonds and Misc. Fixed Income Assets are included on page XR007 of the Health RBC formula. With the implementation of the 20 bond designations and the electronic only tables, the Bonds and Misc. Fixed Income Assets were split between two tabs in the excel file for use of the electronic only tables and ease of printing. However, for increased transparency and system requirements, it is suggested that these pages be split into separate page numbers beginning with year-2021. -
Response of Coastal Water in the Taiwan Strait to Typhoon Nesat of 2017
water Article Response of Coastal Water in the Taiwan Strait to Typhoon Nesat of 2017 Renhao Wu 1,2 , Qinghua Yang 1,3 , Di Tian 4, Bo Han 1,2, Shimei Wu 1,2 and Han Zhang 4,* 1 School of Atmospheric Sciences, and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Zhuhai 519082, China; [email protected] (R.W.); [email protected] (Q.Y.); [email protected] (B.H.); [email protected] (S.W.) 2 Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China 3 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100039, China 4 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; [email protected] * Correspondence: [email protected] Received: 29 September 2019; Accepted: 4 November 2019; Published: 7 November 2019 Abstract: The oceanic response of the Taiwan Strait (TWS) to Typhoon Nesat (2017) was investigated using a fully coupled atmosphere-ocean-wave model (COAWST) verified by observations. Ocean currents in the TWS changed drastically in response to significant wind variation during the typhoon. The response of ocean currents was characterised by a flow pattern generally consistent with the Ekman boundary layer theory, with north-eastward volume transport being significantly modified by the storm. Model results also reveal that the western TWS experienced the maximum generated storm surge, whereas the east side experienced only moderate storm surge.