A Climatology of Tropical Cyclone Size in the Western North Pacific Using an Alternative Metric Thomas B
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Climate Change and Human Health: Risks and Responses
Climate change and human health RISKS AND RESPONSES Editors A.J. McMichael The Australian National University, Canberra, Australia D.H. Campbell-Lendrum London School of Hygiene and Tropical Medicine, London, United Kingdom C.F. Corvalán World Health Organization, Geneva, Switzerland K.L. Ebi World Health Organization Regional Office for Europe, European Centre for Environment and Health, Rome, Italy A.K. Githeko Kenya Medical Research Institute, Kisumu, Kenya J.D. Scheraga US Environmental Protection Agency, Washington, DC, USA A. Woodward University of Otago, Wellington, New Zealand WORLD HEALTH ORGANIZATION GENEVA 2003 WHO Library Cataloguing-in-Publication Data Climate change and human health : risks and responses / editors : A. J. McMichael . [et al.] 1.Climate 2.Greenhouse effect 3.Natural disasters 4.Disease transmission 5.Ultraviolet rays—adverse effects 6.Risk assessment I.McMichael, Anthony J. ISBN 92 4 156248 X (NLM classification: WA 30) ©World Health Organization 2003 All rights reserved. Publications of the World Health Organization can be obtained from Marketing and Dis- semination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; email: [email protected]). Requests for permission to reproduce or translate WHO publications—whether for sale or for noncommercial distribution—should be addressed to Publications, at the above address (fax: +41 22 791 4806; email: [email protected]). The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Estimates of Tropical Cyclone Geometry Parameters Based on Best Track Data
https://doi.org/10.5194/nhess-2019-119 Preprint. Discussion started: 27 May 2019 c Author(s) 2019. CC BY 4.0 License. Estimates of tropical cyclone geometry parameters based on best track data Kees Nederhoff1, Alessio Giardino1, Maarten van Ormondt1, Deepak Vatvani1 1Deltares, Marine and Coastal Systems, Boussinesqweg 1, 2629 HV Delft, The Netherlands 5 Correspondence to: Kees Nederhoff ([email protected]) Abstract. Parametric wind profiles are commonly applied in a number of engineering applications for the generation of tropical cyclone (TC) wind and pressure fields. Nevertheless, existing formulations for computing wind fields often lack the required accuracy when the TC geometry is not known. This may affect the accuracy of the computed impacts generated by these winds. In this paper, empirical stochastic relationships are derived to describe two important parameters affecting the 10 TC geometry: radius of maximum winds (RMW) and the radius of gale force winds (∆AR35). These relationships are formulated using best track data (BTD) for all seven ocean basins (Atlantic, S/NW/NE Pacific, N/SW/SE Indian Oceans). This makes it possible to a) estimate RMW and ∆AR35 when these properties are not known and b) generate improved parametric wind fields for all oceanic basins. Validation results show how the proposed relationships allow the TC geometry to be represented with higher accuracy than when using relationships available from literature. Outer wind speeds can be 15 well reproduced by the commonly used Holland wind profile when calibrated using information either from best-track-data or from the proposed relationships. The scripts to compute the TC geometry and the outer wind speed are freely available via the following URL. -
Aristotle University of Thessaloniki School of Geology Department of Meteorology and Climatology
1 ARISTOTLE UNIVERSITY OF THESSALONIKI SCHOOL OF GEOLOGY DEPARTMENT OF METEOROLOGY AND CLIMATOLOGY School of Geology 541 24 – Thessaloniki Greece Tel: 2310-998240 Fax:2310995392 e-mail: [email protected] 25 August 2020 Dear Editor We have submitted our revised manuscript with title “Fast responses on pre- industrial climate from present-day aerosols in a CMIP6 multi-model study” for potential publication in Atmospheric Chemistry and Physics. We considered all the comments of the reviewers and there is a detailed response on their comments point by point (see below). I would like to mention that after uncovering an error in the set- up of the atmosphere-only configuration of UKESM1, the piClim simulations of UKESM1-0-LL were redone and uploaded on ESGF (O'Connor, 2019a,b). Hence all ensemble calculations and Figures were redone using the new UKESM1-0-LL simulations. Furthermore, a new co-author (Konstantinos Tsigaridis), who has contributed in the simulations of GISS-E2-1-G used in this work, was added in the manuscript. Yours sincerely Prodromos Zanis Professor 2 Reply to Reviewer #1 We would like to thank Reviewer #1 for the constructive and helpful comments. Reviewer’s contribution is recognized in the acknowledgments of the revised manuscript. It follows our response point by point. 1) The Reviewer notes: “Section 1: Fast response vs. slow response discussion. I understand the use of these concepts, especially in view of intercomparing models. Imagine you have to talk to a wider audience interested in the “effective response” of climate to aerosol forcing in a naturally coupled climate system. -
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. -
Cruising Guide to the Philippines
Cruising Guide to the Philippines For Yachtsmen By Conant M. Webb Draft of 06/16/09 Webb - Cruising Guide to the Phillippines Page 2 INTRODUCTION The Philippines is the second largest archipelago in the world after Indonesia, with around 7,000 islands. Relatively few yachts cruise here, but there seem to be more every year. In most areas it is still rare to run across another yacht. There are pristine coral reefs, turquoise bays and snug anchorages, as well as more metropolitan delights. The Filipino people are very friendly and sometimes embarrassingly hospitable. Their culture is a unique mixture of indigenous, Spanish, Asian and American. Philippine charts are inexpensive and reasonably good. English is widely (although not universally) spoken. The cost of living is very reasonable. This book is intended to meet the particular needs of the cruising yachtsman with a boat in the 10-20 meter range. It supplements (but is not intended to replace) conventional navigational materials, a discussion of which can be found below on page 16. I have tried to make this book accurate, but responsibility for the safety of your vessel and its crew must remain yours alone. CONVENTIONS IN THIS BOOK Coordinates are given for various features to help you find them on a chart, not for uncritical use with GPS. In most cases the position is approximate, and is only given to the nearest whole minute. Where coordinates are expressed more exactly, in decimal minutes or minutes and seconds, the relevant chart is mentioned or WGS 84 is the datum used. See the References section (page 157) for specific details of the chart edition used. -
Effects of Landfall Location and the Approach Angle of a Cyclone Vortex Encountering a Mesoscale Mountain Range
SEPTEMBER 2011 L I N A N D S A V A G E 2095 Effects of Landfall Location and the Approach Angle of a Cyclone Vortex Encountering a Mesoscale Mountain Range YUH-LANG LIN Department of Physics, and Department of Energy & Environmental Systems, and NOAA ISET Center, North Carolina A&T State University, Greensboro, North Carolina L. CROSBY SAVAGE III Wind Analytics, WindLogics, Inc., St. Paul, Minnesota (Manuscript received 3 November 2010, in final form 30 April 2011) ABSTRACT The orographic effects of landfall location, approach angle, and their combination on track deflection during the passage of a cyclone vortex over a mesoscale mountain range are investigated using idealized model simulations. For an elongated mesoscale mountain range, the local vorticity generation, driving the cyclone vortex track deflection, is more dominated by vorticity advection upstream of the mountain range, by vorticity stretching over the lee side and its immediate downstream area, and by vorticity advection again far downstream of the mountain as it steers the vortex back to its original direction of movement. The vorticity advection upstream of the mountain range is caused by the flow splitting associated with orographic blocking. It is found that the ideally simulated cyclone vortex tracks compare reasonably well with observed tracks of typhoons over Taiwan’s Central Mountain Range (CMR). In analyzing the relative vorticity budget, the authors found that jumps in the vortex path are largely governed by stretching on the lee side of the mountain. Based on the vorticity equation, this stretching occurs where fluid columns descend the lee slope so that the rate of stretching is governed mostly by the flow speed and the terrain slope. -
Geography and Atmospheric Science 1
Geography and Atmospheric Science 1 Undergraduate Research Center is another great resource. The center Geography and aids undergraduates interested in doing research, offers funding opportunities, and provides step-by-step workshops which provide Atmospheric Science students the skills necessary to explore, investigate, and excel. Atmospheric Science labs include a Meteorology and Climate Hub Geography as an academic discipline studies the spatial dimensions of, (MACH) with state-of-the-art AWIPS II software used by the National and links between, culture, society, and environmental processes. The Weather Service and computer lab and collaborative space dedicated study of Atmospheric Science involves weather and climate and how to students doing research. Students also get hands-on experience, those affect human activity and life on earth. At the University of Kansas, from forecasting and providing reports to university radio (KJHK 90.7 our department's programs work to understand human activity and the FM) and television (KUJH-TV) to research project opportunities through physical world. our department and the University of Kansas Undergraduate Research Center. Why study geography? . Because people, places, and environments interact and evolve in a changing world. From conservation to soil science to the power of Undergraduate Programs geographic information science data and more, the study of geography at the University of Kansas prepares future leaders. The study of geography Geography encompasses landscape and physical features of the planet and human activity, the environment and resources, migration, and more. Our Geography integrates information from a variety of sources to study program (http://geog.ku.edu/degrees/) has a unique cross-disciplinary the nature of culture areas, the emergence of physical and human nature with pathway options (http://geog.ku.edu/geography-pathways/) landscapes, and problems of interaction between people and the and diverse faculty (http://geog.ku.edu/faculty/) who are passionate about environment. -
Improvement of Wind Field Hindcasts for Tropical Cyclones
Water Science and Engineering 2016, 9(1): 58e66 HOSTED BY Available online at www.sciencedirect.com Water Science and Engineering journal homepage: http://www.waterjournal.cn Improvement of wind field hindcasts for tropical cyclones Yi Pan a,b, Yong-ping Chen a,b,*, Jiang-xia Li a,b, Xue-lin Ding a,b a State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China b College of Harbor, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, China Received 16 August 2015; accepted 10 December 2015 Available online 21 February 2016 Abstract This paper presents a study on the improvement of wind field hindcasts for two typical tropical cyclones, i.e., Fanapi and Meranti, which occurred in 2010. The performance of the three existing models for the hindcasting of cyclone wind fields is first examined, and then two modification methods are proposed to improve the hindcasted results. The first one is the superposition method, which superposes the wind field calculated from the parametric cyclone model on that obtained from the cross-calibrated multi-platform (CCMP) reanalysis data. The radius used for the superposition is based on an analysis of the minimum difference between the two wind fields. The other one is the direct modification method, which directly modifies the CCMP reanalysis data according to the ratio of the measured maximum wind speed to the reanalyzed value as well as the distance from the cyclone center. Using these two methods, the problem of underestimation of strong winds in reanalysis data can be overcome. Both methods show considerable improvements in the hindcasting of tropical cyclone wind fields, compared with the cyclone wind model and the reanalysis data. -
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). -
NASA COP 22 Hyperwall Brochure 2016
United Nations Framework Convention on Climate Change NASA Hyperwall Science Stories Hyperwall Stories are Available for Download at: svs.gsfc.nasa.gov/hw Cover Image: SeaWIFS Full Mission Composite SeaStar, SeaWiFS, Chlorophyll Concentration Table of Contents Observing Earth from Space ...................................................................... 3 Changes at Earth’s Poles ............................................................................ 9 Water in the Earth System ......................................................................... 15 Earth’s Atmosphere .................................................................................... 37 Forests and Biodiversity ............................................................................. 45 Human Footprints ...................................................................................... 51 Observing Earth from Space Current Earth Science Satellite Missions In order to study the Earth as a whole system and understand how it is changing, NASA develops and supports a large number of Earth observing missions. These missions provide Earth science researchers the necessary data to address key questions about global climate change. Missions begin with a study phase during which the key science objectives of the mission are identified, and designs for spacecraft and instruments are analyzed. Following a successful study phase, missions enter a development phase whereby all aspects of the mission are developed and tested to insure it meets the mission objectives. -
Hurricane Flooding
ATM 10 Severe and Unusual Weather Prof. Richard Grotjahn L 18/19 http://canvas.ucdavis.edu Lecture 18 topics: • Hurricanes – what is a hurricane – what conditions favor their formation? – what is the internal hurricane structure? – where do they occur? – why are they important? – when are those conditions met? – what are they called? – What are their life stages? – What does the ranking mean? – What causes the damage? Time lapse of the – (Reading) Some notorious storms 2005 Hurricane Season – How to stay safe? Note the water temperature • Video clips (colors) change behind hurricanes (black tracks) (Hurricane-2005_summer_clouds-SST.mpg) Reading: Notorious Storms • Atlantic hurricanes are referred to by name. – Why? • Notorious storms have their name ‘retired’ © AFP Notorious storms: progress and setbacks • August-September 1900 Galveston, Texas: 8,000 dead, the deadliest in U.S. history. • September 1906 Hong Kong: 10,000 dead. • September 1928 South Florida: 1,836 dead. • September 1959 Central Japan: 4,466 dead. • August 1969 Hurricane Camille, Southeast U.S.: 256 dead. • November 1970 Bangladesh: 300,000 dead. • April 1991 Bangladesh: 70,000 dead. • August 1992 Hurricane Andrew, Florida and Louisiana: 24 dead, $25 billion in damage. • October/November 1998 Hurricane Mitch, Honduras: ~20,000 dead. • August 2005 Hurricane Katrina, FL, AL, MS, LA: >1800 dead, >$133 billion in damage • May 2008 Tropical Cyclone Nargis, Burma (Myanmar): >146,000 dead. Some Notorious (Atlantic) Storms Tracks • Camille • Gilbert • Mitch • Andrew • Not shown: – 2004 season (Charley, Frances, Ivan, Jeanne) – Katrina (Wilma & Rita) (2005) – Sandy (2012), Harvey (2017), Florence & Michael (2018) Hurricane Camille • 14-19 August 1969 • Category 5 at landfall – for 24 hours – peak winds 165 kts (190mph @ landfall) – winds >155kts for 18 hrs – min SLP 905 mb (26.73”) – 143 perished along gulf coast, – another 113 in Virginia Hurricane Andrew • 23-26 August 1992 • Category 5 at landfall • first Category 5 to hit US since Camille • affected S. -
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