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Enhancing Psychological Support
Appeal No. MDRCN001 CHINA: FLOODS 2006 17 October 2007 The Federation’s mission is to improve the lives of vulnerable people by mobilizing the power of humanity. It is the world’s largest humanitarian organization and its millions of volunteers are active in over 185 countries. In Brief Final Report; Period covered: 2 August 2006 - 31 July 2007; Final appeal coverage: 26%. <Click here to link directly to the attached Final Financial Report>. Appeal history: • This appeal was launched on 02 August 2006 seeking CHF 5,950,200 (USD 4,825,791 or EUR 3,782,708) for 12 months to assist 240,000 beneficiaries. • Disaster Relief Emergency Funds (DREF) allocated: CHF 213,000 Related Emergency or Annual Appeals: 2006-2007 China Appeal MAACN001 2006-2007 East Asia Appeal MAA54001 Operational Summary: Every year, China is crippled by various natural disasters. In 2006, natural disasters were responsible for the deaths of at least 3,186 people. Over 13.8 million people were evacuated and relocated, with 1.93 million houses completely destroyed. According to latest statistics provided by the ministry of civil affairs, flooding in 2006 had caused a direct economic loss of USD 24 billion (CHF 30 billion). The Red Cross Society of China first responded to meet the emergency needs in Hunan province arising from typhoon Bilis. The Disaster Relief Emergency Fund allocated CHF 213,000 to initial relief distributions. A flood affected village in Hunan province. RCSC/International Federation Through the Federation’s China Floods Emergency Appeal (MDRCN001) launched on 2 August 2006, CHF 1.57 million was raised to provide additional support to beneficiaries through the national society. -
ABSTRACT Title of Dissertation: the GENESIS of TYPHOON
ABSTRACT Title of Dissertation: THE GENESIS OF TYPHOON CHANCHU (2006) Wallace A. Hogsett, Ph.D., 2010 Directed By: Professor Da-Lin Zhang Department of Atmospheric and Oceanic Science The phenomenon of tropical cyclogenesis (TCG), defined as the processes by which common tropical convection organizes into a coherent, self-sustaining, rapidly- rotating, and potentially destructive tropical cyclone (TC), consistently headlines research efforts but still remains largely mysterious. TCG has been described by a leading TC scientist as “one of the great remaining mysteries of the tropical atmosphere.” This dissertation was motivated by a specific case of TCG: the near- equatorial formation of a well-organized synoptic cyclonic disturbance during the active West Pacific Madden-Julian Oscillation (MJO). At very high resolution, the Weather Research and Forecasting (WRF) mesoscale atmospheric model proves capable of reproducing the multiscale interactions that comprise the TCG of Typhoon Chanchu. In the first part of the dissertation, the synoptic observations of the incipient disturbance (i.e., weak cyclonic vortex) are compared with the results from the WRF simulation. It is found that the disturbance tilts westward with height, and as a consequence of the vertical tilt, large-scale ascent (and thus precipitation) is dynamically favored on the downtilt-right side of the vortex. A major result is that the precipitation to the north of the tilted vortex serves as an attractor to the vortex through its generation of vorticity, thereby serving to dually diminish the vertical tilt of the vortex and deflect the incipient storm northward. Observations and the model simulation both indicate that TCG commences when the storm becomes vertically upright. -
Meteorology and Climate
Canadian Technical Report of Fisheries and Aquatic Sciences 2667 2007 ECOSYSTEM OVERVIEW: PACIFIC NORTH COAST INTEGRATED MANAGEMENT AREA (PNCIMA) APPENDIX B: METEOROLOGY AND CLIMATE Authors: William Crawford1, Duncan Johannessen2, Rick Birch3, Keith Borg3, and David Fissel3 Edited by: B.G. Lucas, S. Verrin, and R. Brown 1 Fisheries & Oceans Canada, Institute of Ocean Sciences, Sidney, BC V8L 4B2 2 Earth and Ocean Sciences, University of Victoria, PO Box 3055 STN CSC, Victoria, BC V8W 3P6 3 ASL Environmental Sciences, 1986 Mills Road, Sidney, BC V8L 5Y3 © Her Majesty the Queen in right of Canada, 2007. Cat. No. Fs 97-6/2667E ISSN 0706-6457 Correct citation for this publication: Crawford, W., Johannessen, D., Birch, R., Borg, K., and Fissel, D. 2007. Appendix B: Meteorology and climate. In Ecosystem overview: Pacific North Coast Integrated Management Area (PNCIMA). Edited by Lucas, B.G., Verrin, S., and Brown, R. Can. Tech. Rep. Fish. Aquat. Sci. 2667: iv + 18 p. TABLE OF CONTENTS 1.0 INTRODUCTION...........................................................................................................................1 1.1 KEY POINTS ................................................................................................................................1 1.2 UNCERTAINTIES, LIMITATIONS, AND VARIABILITY .....................................................................2 1.3 MAJOR SOURCES OF INFORMATION OR DATA .............................................................................2 1.4 IDENTIFIED KNOWLEDGE AND DATA GAPS .................................................................................3 -
Weather Numbers Multiple Choices I
Weather Numbers Answer Bank A. 1 B. 2 C. 3 D. 4 E. 5 F. 25 G. 35 H. 36 I. 40 J. 46 K. 54 L. 58 M. 72 N. 74 O. 75 P. 80 Q. 100 R. 910 S. 1000 T. 1010 U. 1013 V. ½ W. ¾ 1. Minimum wind speed for a hurricane in mph N 74 mph 2. Flash-to-bang ratio. For every 10 second between lightning flash and thunder, the storm is this many miles away B 2 miles as flash to bang ratio is 5 seconds per mile 3. Minimum diameter of a hailstone in a severe storm (in inches) A 1 inch (formerly ¾ inches) 4. Standard sea level pressure in millibars U 1013.25 millibars 5. Minimum wind speed for a severe storm in mph L 58 mph 6. Minimum wind speed for a blizzard in mph G 35 mph 7. 22 degrees Celsius converted to Fahrenheit M 72 22 x 9/5 + 32 8. Increments between isobars in millibars D 4mb 9. Minimum water temperature in Fahrenheit for hurricane development P 80 F 10. Station model reports pressure as 100, what is the actual pressure in millibars T 1010 (remember to move decimal to left and then add either 10 or 9 100 become 10.0 910.0mb would be extreme low so logic would tell you it would be 1010.0mb) Multiple Choices I 1. A dry line front is also known as a: a. dew point front b. squall line front c. trough front d. Lemon front e. Kelvin front 2. -
Aleutian Islands
Ecosystem Status Report 2018 Aleutian Islands Edited by: Stephani Zador1 and Ivonne Ortiz2 1Resource Ecology and Fisheries Management Division, Alaska Fisheries Science Center, National Marine Fisheries Service, NOAA 7600 Sand Point Way NE, Seattle, WA 98115 2 JISAO, University of Washington, Seattle, WA With contributions from: Sonia Batten, Jennifer Boldt, Nick Bond, Anne Marie Eich, Ben Fissel, Shannon Fitzgerald, Sarah Gaichas, Jerry Hoff, Steve Kasperski, Carol Ladd, Ned Laman, Geoffrey Lang, Jean Lee, Jennifer Mondragon, John Olson,Ivonne Ortiz, Wayne Palsson, Heather Renner, Nora Rojek, Chris Rooper, Kim Sparks, Michelle St Martin, Jordan Watson, George A. Whitehouse, Sarah Wise, and Stephani Zador Reviewed by: The Plan Teams for the Groundfish Fisheries of the Bering Sea, Aleutian Islands, and Gulf of Alaska November 13, 2018 North Pacific Fishery Management Council 605 W. 4th Avenue, Suite 306 Anchorage, AK 99301 Aleutian Islands 2018 Report Card Region-wide The North Pacific Index (NPI) was strongly positive from fall 2017 into 2018 due to the relatively high sea level pressure in the region of the Aleutian Low, which was displaced to the northwest, over Siberia, and caused persistent warm winds from the southwest. Positive NPI is expected during La Ni~na,but its magnitude was greater than expected. The Aleutians Islands region experienced suppressed storminess through fall and winter 2017/2018 across the region. The Alaska Stream appears to have been relatively diffuse on the south side of the eastern Aleutian Islands. Although the sea surface temperatures cooled in 2018, relative to the 2014{2017 warm period, the overall temperature was still warm due to heat retention throughout the water column. -
Review of the Draft Climate Science Special Report
THE NATIONAL ACADEMIES PRESS This PDF is available at http://www.nap.edu/24712 SHARE Review of the Draft Climate Science Special Report DETAILS 132 pages | 8.5 x 11 | PAPERBACK ISBN 978-0-309-45664-7 | DOI: 10.17226/24712 CONTRIBUTORS GET THIS BOOK Committee to Review the Draft Climate Science Special Report; Board on Atmospheric Sciences and Climate; Division on Earth and Life Studies; National Academies of Sciences, Engineering, and FIND RELATED TITLES Medicine 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. Review of the Draft Climate Science Special Report Committee to Review the Draft Climatee Science Special Report Board on Atmospheric Sciences and Climate Division on Earth and Life Studies A Report of Copyright © National Academy of Sciences. All rights reserved. Review of the Draft Climate Science Special Report THE NATIONAL ACADEMIES PRESS 500 Fifth Street, NW Washington, DC 20001 This study was supported by the National Aeronautics and Space Administration under award numbers NNH14CK78B and NNH14CK79D. Any opinions, findings, conclusions, or recommendations expressed in this publication do not necessarily reflect the views of any organization or agency that provided support for the project. -
Philippines: Typhoon Fengshen
Emergency appeal n° MDRPH004 Philippines: GLIDE n° TC-2008-000093-PHL Operations update n° 4 31 December 2008 Typhoon Fengshen Period covered by this Ops Update: 24 September to 15 December 2008 Appeal target (current): CHF 8,310,213 (USD 8 million or EUR 5.1 million); with this Operations Update, the appeal has been revised to CHF 1,996,287 (USD 1,878,149 or EUR 1,343,281) <click here to view the attached Revised Emergency Appeal Budget> Appeal coverage: To date, the appeal is 87%. Funds are urgently needed to enable the Philippine National Red Cross to provide assistance to those affected by the typhoon.; <click here to go directly to the updated donor response A transitional shelter house in the midst of being built in the municipality of report, or here to link to contact Santa Barbara, Ilo Ilo province. Photo: Philippine National Red Cross. details > Appeal history: • A preliminary emergency appeal was launched on 24 June 2008 for CHF 8,310,213 (USD 8 million or EUR 5.1 million) for 12 months to assist 6,000 families. • Disaster Relief Emergency Fund (DREF): CHF 200,000 was allocated from the International Federation’s DREF. Summary: The onslaught of typhoon Fengshen which hit the Philippines on 18 June 2008, followed by floods and landslides, have left in its wake urgent needs among poverty-stricken communities. According to the National Disaster Coordinating Council (NDCC), approximately four million people have been affected through out the country by typhoon Fengshen. More than 81,000 houses were totally destroyed and a further 326,321 seriously damaged. -
Disaster Preparedness Level, Graph Showed the Data in %, Developed on the Basis of Survey Conducted in Region Vi
2014 Figures Nature Begins Where Human Predication Ends Typhoon Frank (Fengshen) 17th to 27th June, 2008 Credit: National Institute of Geological Sciences, University of the Philippines, 2012 Tashfeen Siddique – Research Fellow AIM – Stephen Zuellig Graduate School of Development Management 8/15/2014 Nature Begins Where Human Predication Ends Contents Acronyms and Abbreviations: ...................................................................................................... iv Brief History ........................................................................................................................................ 1 Philippines Climate ........................................................................................................................... 2 Chronology of Typhoon Frank ....................................................................................................... 3 Forecasting went wrong .................................................................................................................. 7 Warning and Precautionary Measures ...................................................................................... 12 Typhoon Climatology-Science ..................................................................................................... 14 How Typhoon Formed? .............................................................................................................. 14 Typhoon Structure ..................................................................................................................... -
Nihongo in Japan Canrm>T Attend? the ’Unfair Advantage' in 4Act, It in the Reverse of Accusations Made I N Tjy' HEN TELEPHONING a Japa- Frus^Fating, FH Tell You
gswe iwia-s «**««* Chapters discMss Japan-bashing —page 20 Pacific^tatkxwl PubecMlkxi of Ihe JoponeseCitizen Amwlcon Cllttore LocigLB . i. (76e Pcwtpoia U4) Norton* 2 3 ISSN 0030-8579 701 East 3rd Siteel, Suite 201. Los Angeles. CA 90013 (213)626-6934 Friday, July 31, August 7,1992 JACL news JACL SCHOLARSfllPS Senate committee refuses to move on redress btil By KAREN K. NARASAKI Washington. O.C. reprasentdive 'Hm Gvil Liberties Act Amend ments of 1992, S. 2553 it pending in the Senate Governmental Af- • Pacific Citizen presents its annual scholarship FRESHMAN Cairt Committee chaired by Sena issue announcing the academic achievements David M. Watanabe tor John Glenn (D-OH). It has not Heiuy and Chiyo Kuwakara Memonal Scholarship come up fm-a hearing because of of students from around the country. We intro $5,000 the continued insistence by the duce some of these OLitstanding students with RasidenM: Omaha, Neb. Office ofiManagerdent and Bud Parents: Mike and Judith Watanabe their photos dnd biographical backgrounds. get (0MB) that the additional School: Colorado State University $320 million being sought not be -Congratulations to them and to the Class of 1992 This number one ranked student (4.05 GPA) at accorded the same treatment un Brownell-Talbot High School in Onaha, says his inte!*est der the Budget Enfmxement Act and baekgrounrjjnarjhave not only helped him develop as the original funds. as a person but wHIgui de hi m i n hi s career asen enp neer. Senates- Cranston (D-CA) has "Wien I was younger and afraid to interact with my agreed to become a co-sponeor. -
Interagency Strategic Research Plan for Tropical Cyclones: the Way Ahead
INTERAGENCY STRATEGIC RESEARCH PLAN FOR TROPICAL CYCLONES THE WAY AHEAD FCM-P36-2007 February 2007 Office of the Federal Coordinator for Meteorological Services and Supporting Research THE FEDERAL COMMITTEE FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH (FCMSSR) VADM CONRAD C. LAUTENBACHER, JR., USN (RET.) MR. RANDOLPH LYON Chairman, Department of Commerce Office of Management and Budget DR. SHARON L. HAYS MS. VICTORIA COX Office of Science and Technology Policy Department of Transportation DR. RAYMOND MOTHA MR. DAVID MAURSTAD Department of Agriculture Federal Emergency Management Agency Department of Homeland Security BRIG GEN DAVID L. JOHNSON, USAF (RET.) Department of Commerce DR. MARY L. CLEAVE National Aeronautics and Space MR. ALAN SHAFFER Administration Department of Defense DR. MARGARET S. LEINEN DR. JERRY ELWOOD National Science Foundation Department of Energy MR. PAUL MISENCIK MR. KEVIN “SPANKY” KIRSCH National Transportation Safety Board Science and Technology Directorate Department of Homeland Security MR. JAMES WIGGINS U.S. Nuclear Regulatory Commission DR. MICHAEL SOUKUP Department of the Interior DR. LAWRENCE REITER Environmental Protection Agency MR. RALPH BRAIBANTI Department of State MR. SAMUEL P. WILLIAMSON Federal Coordinator MR. JAMES B. HARRISON, Executive Secretary Office of the Federal Coordinator for Meteorological Services and Supporting Research THE INTERDEPARTMENTAL COMMITTEE FOR METEOROLOGICAL SERVICES AND SUPPORTING RESEARCH (ICMSSR) MR. SAMUEL P. WILLIAMSON, Chairman MR. JAMES H. WILLIAMS Federal Coordinator Federal Aviation Administration Department of Transportation MR. THOMAS PUTERBAUGH Department of Agriculture DR. JONATHAN M. BERKSON United States Coast Guard MR. JOHN E. JONES, JR. Department of Homeland Security Department of Commerce MR. JEFFREY MACLURE RADM FRED BYUS, USN Department of State United States Navy Department of Defense DR. -
October 2013 Global Catastrophe Recap 2 2
October 2013 Global Catastrophe Recap Table of Contents Executive0B Summary 3 United2B States 4 Remainder of North America (Canada, Mexico, Caribbean, Bermuda) 4 South4B America 4 Europe 4 6BAfrica 5 Asia 5 Oceania8B (Australia, New Zealand and the South Pacific Islands) 6 8BAAppendix 7 Contact Information 14 Impact Forecasting | October 2013 Global Catastrophe Recap 2 2 Executive0B Summary . Windstorm Christian affects western and northern Europe; insured losses expected to top USD1.35 billion . Cyclone Phailin and Typhoon Fitow highlight busy month of tropical cyclone activity in Asia . Deadly bushfires destroy hundreds of homes in Australia’s New South Wales Windstorm Christian moved across western and northern Europe, bringing hurricane-force wind gusts and torrential rains to several countries. At least 18 people were killed and dozens more were injured. The heaviest damage was sustained in the United Kingdom, France, Belgium, the Netherlands and Scandinavia, where a peak wind gust of 195 kph (120 mph) was recorded in Denmark. More than 1.2 million power outages were recorded and travel was severely disrupted throughout the continent. Reports from European insurers suggest that payouts are likely to breach EUR1.0 billion (USD1.35 billion). Total economic losses will be even higher. Christian becomes the costliest European windstorm since WS Xynthia in 2010. Cyclone Phailin became the strongest system to make landfall in India since 1999, coming ashore in the eastern state of Odisha. At least 46 people were killed. Tremendous rains, an estimated 3.5-meter (11.0-foot) storm surge, and powerful winds led to catastrophic damage to more than 430,000 homes and 668,000 hectares (1.65 million) acres of cropland. -
Initializing the WRF Model with Tropical Cyclone Real-Time Reports Using the Ensemble
Initializing the WRF Model with Tropical Cyclone Real-Time Reports using the Ensemble Kalman Filter Algorithm Tien Duc Du(1), Thanh Ngo-Duc(2), and Chanh Kieu(3)* (1)National Center for Hydro-Meteorological Forecasting, 8 Phao Dai Lang, Hanoi, Vietnam 1 (2)Department of Space and Aeronautics, University of Science and Technology of Hanoi, Vietnam 2 (3)Department of Earth and Atmospheric Sciences, Indiana University, Bloomington IN 47405, USA Revised: 18 April 2017 Submitted to Pure and Applied Geophysical Science Abbreviated title: Tropical Cyclone Ensemble Forecast Keywords: Tropical cyclones, ensemble Kalman filter, the WRF model, tropical cyclone vital, ensemble forecasting ____________________ *Corresponding author: Chanh Kieu, Atmospheric Program, GY428A Geological Building, Department of Earth and Atmospheric Sciences, Indiana University, Bloomington, IN 47405. Tel: 812-856-5704. Email: [email protected]. 1 1 Abstract 2 This study presents an approach to assimilate tropical cyclone (TC) real-time reports and the 3 University of Wisconsin-Cooperative Institute for Meteorological Satellite Studies (CIMSS) 4 Atmospheric Motion Vectors (AMV) data into the Weather Research and Forecasting (WRF) model 5 for TC forecast applications. Unlike current methods in which TC real-time reports are used to either 6 generate a bogus vortex or spin-up a model initial vortex, the proposed approach ingests the TC real- 7 time reports through blending a dynamically consistent synthetic vortex structure with the CIMSS- 8 AMV data. The blended dataset is then assimilated into the WRF initial condition, using the local 9 ensemble transform Kalman filter (LETKF) algorithm. Retrospective experiments for a number of 10 TC cases in the north Western Pacific basin during 2013-2014 demonstrate that this approach could 11 effectively increase both the TC circulation and enhance the large-scale environment that the TCs are 12 embedded in.