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Characteristics of Satellite-Based Ocean Turbulent Heat Flux Around the Korean Peninsula and Relationship with Changes in Typhoon Intensity
remote sensing Article Characteristics of Satellite-Based Ocean Turbulent Heat Flux around the Korean Peninsula and Relationship with Changes in Typhoon Intensity Jaemin Kim and Yun Gon Lee * Atmospheric Sciences, Department of Astronomy, Space Science, and Geology, Chungnam National University, Daejeon 34134, Korea; [email protected] * Correspondence: [email protected]; Tel.: +82-042-821-7107 Abstract: Ocean-atmosphere energy exchange is an important factor in the maintenance of oceanic and atmospheric circulation and the regulation of meteorological and climate systems. Oceanic sensible and latent heat fluxes around the Korean Peninsula were determined using satellite-based air-sea variables (wind speed, sea surface temperature, and atmospheric specific humidity and temperature) and the coupled ocean-atmosphere response experiment (COARE) 3.5 bulk algorithm for six years between 2014 and 2019. Seasonal characteristics of the marine heat flux and its short- term fluctuations during summer typhoons were also investigated. Air-sea variables were produced through empirical relationships and verified with observational data from marine buoys around the Korean Peninsula. Satellite-derived wind speed, sea surface temperature, atmospheric specific humidity, and air temperature were strongly correlated with buoy data, with R2 values of 0.80, 0.97, 0.90, and 0.91, respectively. Satellite-based sensible and latent heat fluxes around the peninsula were also validated against fluxes calculated from marine buoy data, and displayed low values in summer and higher values in autumn and winter as the difference between air-sea temperature and specific humidity increased. Through analyses of spatio-temporal fluctuations in the oceanic turbulent heat Citation: Kim, J.; Lee, Y.G. -
NASA Catches the Eye of Typhoon Lingling 5 September 2019
NASA catches the eye of Typhoon Lingling 5 September 2019 Warning Center or JTWC said that Typhoon Lingling, known locally in the Philippines as Liwayway, had moved away from the Philippines enough that warnings have been dropped. Lingling was located near 23.0 degrees north latitude and 125.4 degrees east longitude. That is 247 nautical miles southwest of Kadena Air Base, Okinawa, Japan. Lingling was moving to the north- northeast and maximum sustained winds had increased to near 80 knots (75 mph/120.3 kph). JTWC forecasters said that Lingling is moving north and is expected to intensify to 105 knots (121 mph/194 kph) upon passing between Taiwan and Japan. Provided by NASA's Goddard Space Flight Center On Sept. 4, 2019 at 1:20 a.m. EDT (0520 UTC) the MODIS instrument that flies aboard NASA's Terra satellite showed powerful thunderstorms circling Typhoon Lingling's visible eye. Credit: NASA/NRL Typhoon Lingling continues to strengthen in the Northwestern Pacific Ocean and NASA's Terra satellite imagery revealed the eye is now visible. On Sept. 4 at 1:20 a.m. EDT (0520 UTC) the Moderate Imaging Spectroradiometer or MODIS instrument that flies aboard NASA's Terra satellite showed powerful thunderstorms circling Typhoon Lingling's visible 15 nautical-mile wide eye. The Joint Typhoon Warning Center (JTWC) noted, "Animated enhanced infrared satellite imagery depicts tightly-curved banding wrapping into a ragged eye." In addition, microwave satellite imagery showed a well-defined microwave eye feature. At 11 a.m. EDT (1500 UTC), the Joint Typhoon 1 / 2 APA citation: NASA catches the eye of Typhoon Lingling (2019, September 5) retrieved 2 October 2021 from https://phys.org/news/2019-09-nasa-eye-typhoon-lingling.html This document is subject to copyright. -
Strategic Plan 2021-2025
Strategic Plan 2021-2025 Map of FSM 2 Contents Map of FSM ___________________________________________________________________________________________________________________ 2 Key Issues in the FSM________________________________________________________________________________________________________ 4 Country Context _____________________________________________________________________________________________________________ 7 Major Vulnerability and Hazards Analysis _________________________________________________________________________________ 8 History of Micronesia Red Cross Society (MRCS) __________________________________________________________________________ 9 IFRC Strategy 2030 _________________________________________________________________________________________________________ 11 MRCS Vision _________________________________________________________________________________________________________________ 12 MRCS Mission: ______________________________________________________________________________________________________________ 12 Strategic Aims 2021-2025 _________________________________________________________________________________________________ 13 Strategic Aim 1: Save lives in times of disasters and crises ______________________________________________________________ 14 Strategic Aim 2: Enable healthy and safe living ___________________________________________________________________________ 16 Strategic Aim 3: Promote the prevention and reduction of vulnerability, social inclusion and a culture of non- violence -
Spatial Variations in Fertility of South Korea: a Geographically Weighted Regression Approach
International Journal of Geo-Information Article Spatial Variations in Fertility of South Korea: A Geographically Weighted Regression Approach Myunggu Jung 1 , Woorim Ko 2, Yeohee Choi 3 and Youngtae Cho 2,* 1 Department of Population Health, London School of Hygiene and Tropical Medicine, London WC1E 7HT, UK; [email protected] 2 Department of Public Health Science, Graduate School of Public Health, Seoul National University, Seoul 08826, Korea; [email protected] 3 Department of Social Welfare, Graduate School of Social Welfare, Ewha Womans University, Seoul 03760, Korea; [email protected] * Correspondence: [email protected]; Tel.: +82-2-880-2820 Received: 5 May 2019; Accepted: 4 June 2019; Published: 5 June 2019 Abstract: South Korea has witnessed a remarkable decline in birth rates in the last few decades. Although there has been a large volume of literature exploring the determinants of low fertility in South Korea, studies on spatial variations in fertility are scarce. This study compares the Ordinary Least Squares (OLS) and Geographically Weighted Regression (GWR) models to investigate the potential role of the spatially heterogeneous response of the total fertility rate (TFR) to sociodemographic factors. The study finds that the relationships between sociodemographic factors and TFRs in South Korea vary across 252 sub-administrative areas in terms of both magnitude and direction. This study therefore demonstrates the value of using spatial analysis for providing evidence-based local-population policy options in pursuit of a fertility rebound in South Korea. Keywords: low fertility; spatial analysis; GIS; regional fertility differentials; total fertility rate 1. Introduction In the last few decades, South Korea has witnessed a remarkable decline in birth rates. -
Lecture 15 Hurricane Structure
MET 200 Lecture 15 Hurricanes Last Lecture: Atmospheric Optics Structure and Climatology The amazing variety of optical phenomena observed in the atmosphere can be explained by four physical mechanisms. • What is the structure or anatomy of a hurricane? • How to build a hurricane? - hurricane energy • Hurricane climatology - when and where Hurricane Katrina • Scattering • Reflection • Refraction • Diffraction 1 2 Colorado Flood Damage Hurricanes: Useful Websites http://www.wunderground.com/hurricane/ http://www.nrlmry.navy.mil/tc_pages/tc_home.html http://tropic.ssec.wisc.edu http://www.nhc.noaa.gov Hurricane Alberto Hurricanes are much broader than they are tall. 3 4 Hurricane Raymond Hurricane Raymond 5 6 Hurricane Raymond Hurricane Raymond 7 8 Hurricane Raymond: wind shear Typhoon Francisco 9 10 Typhoon Francisco Typhoon Francisco 11 12 Typhoon Francisco Typhoon Francisco 13 14 Typhoon Lekima Typhoon Lekima 15 16 Typhoon Lekima Hurricane Priscilla 17 18 Hurricane Priscilla Hurricanes are Tropical Cyclones Hurricanes are a member of a family of cyclones called Tropical Cyclones. West of the dateline these storms are called Typhoons. In India and Australia they are called simply Cyclones. 19 20 Hurricane Isaac: August 2012 Characteristics of Tropical Cyclones • Low pressure systems that don’t have fronts • Cyclonic winds (counter clockwise in Northern Hemisphere) • Anticyclonic outflow (clockwise in NH) at upper levels • Warm at their center or core • Wind speeds decrease with height • Symmetric structure about clear "eye" • Latent heat from condensation in clouds primary energy source • Form over warm tropical and subtropical oceans NASA VIIRS Day-Night Band 21 22 • Differences between hurricanes and midlatitude storms: Differences between hurricanes and midlatitude storms: – energy source (latent heat vs temperature gradients) - Winter storms have cold and warm fronts (asymmetric). -
Tinamiformes – Falconiformes
LIST OF THE 2,008 BIRD SPECIES (WITH SCIENTIFIC AND ENGLISH NAMES) KNOWN FROM THE A.O.U. CHECK-LIST AREA. Notes: "(A)" = accidental/casualin A.O.U. area; "(H)" -- recordedin A.O.U. area only from Hawaii; "(I)" = introducedinto A.O.U. area; "(N)" = has not bred in A.O.U. area but occursregularly as nonbreedingvisitor; "?" precedingname = extinct. TINAMIFORMES TINAMIDAE Tinamus major Great Tinamou. Nothocercusbonapartei Highland Tinamou. Crypturellus soui Little Tinamou. Crypturelluscinnamomeus Thicket Tinamou. Crypturellusboucardi Slaty-breastedTinamou. Crypturellus kerriae Choco Tinamou. GAVIIFORMES GAVIIDAE Gavia stellata Red-throated Loon. Gavia arctica Arctic Loon. Gavia pacifica Pacific Loon. Gavia immer Common Loon. Gavia adamsii Yellow-billed Loon. PODICIPEDIFORMES PODICIPEDIDAE Tachybaptusdominicus Least Grebe. Podilymbuspodiceps Pied-billed Grebe. ?Podilymbusgigas Atitlan Grebe. Podicepsauritus Horned Grebe. Podicepsgrisegena Red-neckedGrebe. Podicepsnigricollis Eared Grebe. Aechmophorusoccidentalis Western Grebe. Aechmophorusclarkii Clark's Grebe. PROCELLARIIFORMES DIOMEDEIDAE Thalassarchechlororhynchos Yellow-nosed Albatross. (A) Thalassarchecauta Shy Albatross.(A) Thalassarchemelanophris Black-browed Albatross. (A) Phoebetriapalpebrata Light-mantled Albatross. (A) Diomedea exulans WanderingAlbatross. (A) Phoebastriaimmutabilis Laysan Albatross. Phoebastrianigripes Black-lootedAlbatross. Phoebastriaalbatrus Short-tailedAlbatross. (N) PROCELLARIIDAE Fulmarus glacialis Northern Fulmar. Pterodroma neglecta KermadecPetrel. (A) Pterodroma -
Field Investigations of Coastal Sea Surface Temperature Drop
1 Field Investigations of Coastal Sea Surface Temperature Drop 2 after Typhoon Passages 3 Dong-Jiing Doong [1]* Jen-Ping Peng [2] Alexander V. Babanin [3] 4 [1] Department of Hydraulic and Ocean Engineering, National Cheng Kung University, Tainan, 5 Taiwan 6 [2] Leibniz Institute for Baltic Sea Research Warnemuende (IOW), Rostock, Germany 7 [3] Department of Infrastructure Engineering, Melbourne School of Engineering, University of 8 Melbourne, Australia 9 ---- 10 *Corresponding author: 11 Dong-Jiing Doong 12 Email: [email protected] 13 Tel: +886 6 2757575 ext 63253 14 Add: 1, University Rd., Tainan 70101, Taiwan 15 Department of Hydraulic and Ocean Engineering, National Cheng Kung University 16 -1- 1 Abstract 2 Sea surface temperature (SST) variability affects marine ecosystems, fisheries, ocean primary 3 productivity, and human activities and is the primary influence on typhoon intensity. SST drops 4 of a few degrees in the open ocean after typhoon passages have been widely documented; 5 however, few studies have focused on coastal SST variability. The purpose of this study is to 6 determine typhoon-induced SST drops in the near-coastal area (within 1 km of the coast) and 7 understand the possible mechanism. The results of this study were based on extensive field data 8 analysis. Significant SST drop phenomena were observed at the Longdong buoy in northeastern 9 Taiwan during 43 typhoons over the past 20 years (1998~2017). The mean SST drop (∆SST) 10 after a typhoon passage was 6.1 °C, and the maximum drop was 12.5 °C (Typhoon Fungwong 11 in 2008). -
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. -
Quantification of Typhoon-Induced Phytoplankton Blooms Using
remote sensing Article Quantification of Typhoon-Induced Phytoplankton Blooms Using Satellite Multi-Sensor Data Jiayi Pan 1,2,3,* ID , Lei Huang 2, Adam T. Devlin 2 and Hui Lin 2 1 School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China 2 Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Hong Kong, China; [email protected] (L.H.); [email protected] (A.T.D.); [email protected] (H.L.) 3 Shenzhen Research Institute, The Chinese University of Hong Kong, Shenzhen 518057, China * Correspondence: [email protected]; Tel.: +852-3943-1308 Received: 19 December 2017; Accepted: 16 February 2018; Published: 20 February 2018 Abstract: Using satellite-based multi-sensor observations, this study investigates Chl-a blooms induced by typhoons in the Northwest Pacific (NWP) and the South China Sea (SCS), and quantifies the blooms via wind-induced mixing and Ekman pumping parameters, as well as pre-typhoon mixed-layer depth (MLD). In the NWP, the Chl-a bloom is more correlated with the Ekman pumping than with the other two parameters, with an R2 value of 0.56. In the SCS, the wind-induced mixing and Ekman pumping have comparable correlations with the Chl-a increase, showing R2 values of 0.4~0.6. However, the MLD exhibits a negative correlation with the Chl-a increase. A multi-parameter quantification model of the Chl-a bloom strength achieves better results than the single-parameter regressions, yielding a more significant R2 value of 0.80, and a lower regression rms of 0.18 mg·m−3 in the SCS, and the R2 value in the NWP is also improved compared with the single-parameter regressions. -
FEMA Daily Situation Report
The Disaster Center is dedicated to the idea that disaster mitigation is cost effective and individuals pursuing their own interest are the greatest potential force for disaster reduction. Please consider making a small donation to the Disaster Center When disaster mitigation is cost effective, we are on the road to bringing disasters to an end. •Daily Operations Briefing Friday, October 18, 2013 8:30 a.m. EDT 1 Significant Activity: Oct 17 – 18 Significant Events: None Tropical Activity: • Atlantic – Tropical cyclone activity is not expected during the next 48 hours • Eastern Pacific – Area 1 (20%) • Central Pacific – Area 1 (10%) • Western Pacific – Typhoon Francisco (26W) Significant Weather: • Slight risk of severe thunderstorms – west central Texas • Heavy rainfall – Gulf Coast • Critical Fire Weather Areas / Red Flag Warnings: None • Space Weather: Past 24 hours: Minor/R1 radio blackouts observed; 24 hours: None predicted Earthquake Activity: No significant activity Declaration Activity: • Amendment No. 3 to FEMA-4129-DR-NY • Major Disaster Declaration requests for California, Arizona and the Santa Clara Pueblo 2 Atlantic – Tropical Outlook Updates at 2:00 am/pm and 8:00 am/pm EDT 3 Eastern Pacific – Tropical Outlook http://www.nhc.noaa.gov/gtwo_epac.shtml This product is updated at approximately 5 AM, 11 AM, 5 PM, and 11 PM PDT from May 15 to November 30. Special outlooks may be issued as conditions warrant. 4 Eastern - Area 1 As of 8:00 a.m. EDT • Located 425 miles south of Gulf of Tehuantepec • Producing disorganized showers and thunderstorms • Conducive for slow development during next several days • Probability of tropical cyclone development: • Next 48 hours: Low ( 20%) • Next 5 days: Medium ( 40%) 5 Central Pacific – Tropical Outlook http://www.prh.noaa.gov/hnl/cphc/ This product is updated at approximately 5 AM, 11 AM, 5 PM, and 11 PM PDT from May 15 to November 30. -
Sigma 1/2008
sigma No 1/2008 Natural catastrophes and man-made disasters in 2007: high losses in Europe 3 Summary 5 Overview of catastrophes in 2007 9 Increasing flood losses 16 Indices for the transfer of insurance risks 20 Tables for reporting year 2007 40 Tables on the major losses 1970–2007 42 Terms and selection criteria Published by: Swiss Reinsurance Company Economic Research & Consulting P.O. Box 8022 Zurich Switzerland Telephone +41 43 285 2551 Fax +41 43 285 4749 E-mail: [email protected] New York Office: 55 East 52nd Street 40th Floor New York, NY 10055 Telephone +1 212 317 5135 Fax +1 212 317 5455 The editorial deadline for this study was 22 January 2008. Hong Kong Office: 18 Harbour Road, Wanchai sigma is available in German (original lan- Central Plaza, 61st Floor guage), English, French, Italian, Spanish, Hong Kong, SAR Chinese and Japanese. Telephone +852 2582 5691 sigma is available on Swiss Re’s website: Fax +852 2511 6603 www.swissre.com/sigma Authors: The internet version may contain slightly Rudolf Enz updated information. Telephone +41 43 285 2239 Translations: Kurt Karl (Chapter on indices) CLS Communication Telephone +41 212 317 5564 Graphic design and production: Jens Mehlhorn (Chapter on floods) Swiss Re Logistics/Media Production Telephone +41 43 285 4304 © 2008 Susanna Schwarz Swiss Reinsurance Company Telephone +41 43 285 5406 All rights reserved. sigma co-editor: The entire content of this sigma edition is Brian Rogers subject to copyright with all rights reserved. Telephone +41 43 285 2733 The information may be used for private or internal purposes, provided that any Managing editor: copyright or other proprietary notices are Thomas Hess, Head of Economic Research not removed. -
A Climatology of Tropical Cyclone Size in the Western North Pacific Using an Alternative Metric Thomas B
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2017 A Climatology of Tropical Cyclone Size in the Western North Pacific Using an Alternative Metric Thomas B. (Thomas Brian) McKenzie III Follow this and additional works at the DigiNole: FSU's Digital Repository. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES A CLIMATOLOGY OF TROPICAL CYCLONE SIZE IN THE WESTERN NORTH PACIFIC USING AN ALTERNATIVE METRIC By THOMAS B. MCKENZIE III A Thesis submitted to the Department of Earth, Ocean and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science 2017 Copyright © 2017 Thomas B. McKenzie III. All Rights Reserved. Thomas B. McKenzie III defended this thesis on March 23, 2017. The members of the supervisory committee were: Robert E. Hart Professor Directing Thesis Vasubandhu Misra Committee Member Jeffrey M. Chagnon Committee Member The Graduate School has verified and approved the above-named committee members, and certifies that the thesis has been approved in accordance with university requirements. ii To Mom and Dad, for all that you’ve done for me. iii ACKNOWLEDGMENTS I extend my sincere appreciation to Dr. Robert E. Hart for his mentorship and guidance as my graduate advisor, as well as for initially enlisting me as his graduate student. It was a true honor working under his supervision. I would also like to thank my committee members, Dr. Vasubandhu Misra and Dr. Jeffrey L. Chagnon, for their collaboration and as representatives of the thesis process. Additionally, I thank the Civilian Institution Programs at the Air Force Institute of Technology for the opportunity to earn my Master of Science degree at Florida State University, and to the USAF’s 17th Operational Weather Squadron at Joint Base Pearl Harbor-Hickam, HI for sponsoring my graduate program and providing helpful feedback on the research.