Tropical Storm List

Size: px
Start display at page:

Download "Tropical Storm List"

Transcription

1 Tropical Storm List Tropical-Storms is a mailing list only for those who are professionally active in either the research or forecasting of tropical storms worldwide. Monsoon is a mailing list for those who are professionally active in the research or forecasting of monsoons worldwide.

2 Tropical Cyclogenesis: Operational Forecasting Perspective International Workshop on Tropical Cyclones Jeju Island, South Korea Working group: Chris Landsea (RSMC Miami), Lixion Avila (RSMC Miami), Thierry Dupont (RSMC La Reunion), S. D. Kotal (RSMC New Delhi), and M. Mohapatra (RSMC New Delhi)

3 Accurate tropical cyclone genesis forecasting is important because of The need to provide extended community response planning, especially in remote or large communities The need to provide advisories at extended forecast ranges for offshore and onshore commercial activities The requirement for National Meteorological Services to manage forecasting and reconnaissance resources The potential to reduce future track, intensity, and size errors by more accurately defining the likely genesis location

4 Accurate tropical cyclone genesis forecasting is important because of The need to provide extended community response planning, especially in remote or large communities The need to provide advisories at extended forecast ranges for offshore and onshore commercial activities The requirement for National Meteorological Services to manage forecasting and reconnaissance resources The potential to reduce future track, intensity, and size errors by more accurately defining the likely genesis location

5 Accurate tropical cyclone genesis forecasting is important because of The need to provide extended community response planning, especially in remote or large communities The need to provide advisories at extended forecast ranges for offshore and onshore commercial activities The requirement for National Meteorological Services to manage forecasting and reconnaissance resources The potential to reduce future track, intensity, and size errors by more accurately defining the likely genesis location

6 Accurate tropical cyclone genesis forecasting is important because of The need to provide extended community response planning, especially in remote or large communities The need to provide advisories at extended forecast ranges for offshore and onshore commercial activities The requirement for National Meteorological Services to manage forecasting and reconnaissance resources The potential to reduce future track, intensity, and size errors by more accurately defining the likely genesis location

7 Within the 2010 IWTC report there was a substantial optimism that genesis forecasting was becoming a solvable problem: Both Ensemble Prediction Systems (EPS) and deterministic Numerical Weather Prediction (NWP) models were routinely capturing TC formation. Improvement in formation forecasts from operational numerical models were expected given advances in various aspects of numerical weather prediction systems, which includes increased resolution, improved parameterization schemes, and improved use of observations, especially satellite data to improve initial conditions. However, tropical cyclone genesis forecast continued to remain a challenging aspect of operational forecasting in the major tropical forecasting centers, as there was still no effective systematic approach in place for genesis forecasting, especially with respect to NWP guidance.

8 Within the 2010 IWTC report there was a substantial optimism that genesis forecasting was becoming a solvable problem: Both Ensemble Prediction Systems (EPS) and deterministic Numerical Weather Prediction (NWP) models were routinely capturing TC formation. Improvement in formation forecasts from operational numerical models were expected given advances in various aspects of numerical weather prediction systems, which includes increased resolution, improved parameterization schemes, and improved use of observations, especially satellite data to improve initial conditions. However, tropical cyclone genesis forecast continued to remain a challenging aspect of operational forecasting in the major tropical forecasting centers, as there was still no effective systematic approach in place for genesis forecasting, especially with respect to NWP guidance.

9 Within the 2010 IWTC report there was a substantial optimism that genesis forecasting was becoming a solvable problem: Both Ensemble Prediction Systems (EPS) and deterministic Numerical Weather Prediction (NWP) models were routinely capturing TC formation. Improvement in formation forecasts from operational numerical models were expected given advances in various aspects of numerical weather prediction systems, which includes increased resolution, improved parameterization schemes, and improved use of observations, especially satellite data to improve initial conditions. However, tropical cyclone genesis forecast continued to remain a challenging aspect of operational forecasting in the major tropical forecasting centers, as there was still no effective systematic approach in place for genesis forecasting, especially with respect to NWP guidance.

10 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

11 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

12 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

13 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

14 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

15 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific)

16 Definition of Tropical Cyclone A warm-core, non-frontal synoptic-scale cyclone, originating over tropical or subtropical waters, with organized deep convection and closed surface wind circulation about a well-defined center. - RSMC Miami/Honolulu (Atlantic/Northeast and North Central Pacific) NOTE: No lower bound of sustained winds

17 Various Definitions of Tropical Cyclone RSMC La Reunion (Southwestern Indian Ocean) - the maximum of the average wind speed has to be at least 28 kt before a tropical disturbance can be considered a tropical depression. RSMC New Delhi (North Indian Ocean) - 17 kt. RSMC Fiji and TCWCs of the Southeastern Indian Ocean and Southwestern Pacific Ocean) - 34 kt. RSMC Tokyo (Northwest Pacific Ocean)- has no lower bound wind speed threshold

18 Forecasting Genesis when Definitions Differ Makes intercomparison of genesis across basins problematic Decision of if/when genesis occurs remains subjective Role of human forecaster is crucial for genesis prediction Genesis of Phanfone, 18W, 2014

19 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

20 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

21 Genesis Forecasting: Observations and Analyses A pre-existing disturbance containing abundant deep convection Latitudes poleward ~5 o SST > 26 o C A sufficiently unstable atmosphere & deep layer of moist air

22 Genesis Forecasting: Observations and Analyses (cont.) Small vertical shear of the horizontal wind Upper-tropospheric anticyclonic outflow Enhanced lower tropospheric relative vorticity Appearance of curved banding features in the deep convection Falling surface pressure: 24-hour pressure changes (falls) of usually 3 mb or more

23 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

24 Cossuth et al. (2013) moe.met.fsu.edu/genesis

25 0-48h Tropical Cyclone Formation Probability Schumacher et al. (2009) 0-24h /TROP/TCFP/index.html 24-48h

26 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

27 Examining Global Model Output for Genesis At least one closed isobar (at 4 mb interval) with lowered central pressure Reasonable structure (closed circulation center, warm core, deep vertical extent, non-baroclinic) Longevity of the vortex for at least a day

28 Very Good Global Model Predictions of Genesis GFS forecasts verifying at genesis time of Hurricane Arthur 28

29 Not so Good Global Model Predictions of Genesis GFS forecasts verifying at genesis time of Hurricane Sandy F168 F156 F144 F132 F120 F108 F96 F84 F72 F60 F48 F36 F24 F00

30 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

31 GFS Ensemble-based Probabilities of Genesis

32 Composite track of tropical cyclone before genesis Elsberry et al. (2011a,b)

33 Genesis Predictions Observations and Analyses Statistical Approaches Deterministic Global Models Ensemble Prediction Systems Statistical-Dynamical Hybrid Approaches

34 Tropical Cyclone Genesis Index Predictors: 1) Dvorak classification 2) 850 mb divergence 3) 850 mb vorticity change 4) mb shear 5) 600 mb humidity 6) Deep convection Dunion (2013)

35 Blending deterministic global models for genesis probabilities Halperin et al. (2013) -

36 Blending deterministic global models for genesis probabilities Halperin et al. (2013) -

37 Tropical Weather Outlook

38

39

40

41 Pre-Genesis Tropical Cyclone Advisories at RSMC Miami To be issued for systems with at least a medium likelihood of genesis within 48 h 72 hr track, intensity, size forecast Only to be issued when a Tropical Storm Warning, Hurricane Watch, or Hurricane Warning needed Beginning in 2016 experimentally

42 Example of Pre-Genesis Advisory

43 Possible Recommendations Researchers should develop methods for providing quantitative (probabilistic) genesis prediction guidance via deterministic, ensemble, and statistical-dynamical models Researchers should develop methods for provide methods for providing pre-genesis prediction guidance of TC track, intensity and size via deterministic, ensemble, and statistical-dynamical models RSMCs/TCWCs should explore issuing quantitative genesis predictions to the public RSMCs/TCWCs should explore increasing lead-time of existing quantitative genesis predictions to the public RSMCs/TCWCs should explore the possibility of issuing pregenesis tropical cyclone track, intensity, and size forecasts

44 Possible Recommendations Researchers should develop methods for providing quantitative (probabilistic) genesis prediction guidance via deterministic, ensemble, and statistical-dynamical models Researchers should develop methods for provide methods for providing pre-genesis prediction guidance of TC track, intensity and size via deterministic, ensemble, and statistical-dynamical models RSMCs/TCWCs should explore issuing quantitative genesis predictions to the public RSMCs/TCWCs should explore increasing lead-time of existing quantitative genesis predictions to the public RSMCs/TCWCs should explore the possibility of issuing pregenesis tropical cyclone track, intensity, and size forecasts

45 Possible Recommendations Researchers should develop methods for providing quantitative (probabilistic) genesis prediction guidance via deterministic, ensemble, and statistical-dynamical models Researchers should develop methods for provide methods for providing pre-genesis prediction guidance of TC track, intensity and size via deterministic, ensemble, and statistical-dynamical models RSMCs/TCWCs should explore issuing quantitative genesis predictions to the public RSMCs/TCWCs should explore increasing lead-time of existing quantitative genesis predictions to the public RSMCs/TCWCs should explore the possibility of issuing pregenesis tropical cyclone track, intensity, and size forecasts

46 Possible Recommendations Researchers should develop methods for providing quantitative (probabilistic) genesis prediction guidance via deterministic, ensemble, and statistical-dynamical models Researchers should develop methods for provide methods for providing pre-genesis prediction guidance of TC track, intensity and size via deterministic, ensemble, and statistical-dynamical models RSMCs/TCWCs should explore issuing quantitative genesis predictions to the public RSMCs/TCWCs should explore increasing lead-time of existing quantitative genesis predictions to the public RSMCs/TCWCs should explore the possibility of issuing pregenesis tropical cyclone track, intensity, and size forecasts

47 Possible Recommendations Researchers should develop methods for providing quantitative (probabilistic) genesis prediction guidance via deterministic, ensemble, and statistical-dynamical models Researchers should develop methods for provide methods for providing pre-genesis prediction guidance of TC track, intensity and size via deterministic, ensemble, and statistical-dynamical models RSMCs/TCWCs should explore issuing quantitative genesis predictions to the public RSMCs/TCWCs should explore increasing lead-time of existing quantitative genesis predictions to the public RSMCs/TCWCs should explore the possibility of issuing pregenesis tropical cyclone track, intensity, and size forecasts

48 Tropical Cyclogenesis: Operational Forecasting Perspective International Workshop on Tropical Cyclones Jeju Island, South Korea Working group: Chris Landsea (RSMC Miami), Lixion Avila (RSMC Miami), Thierry Dupont (RSMC La Reunion), S. D. Kotal (RSMC New Delhi), and M. Mohapatra (RSMC New Delhi)

Topic 2: Cyclogenesis, Intensity and Intensity Change

Topic 2: Cyclogenesis, Intensity and Intensity Change EIGHTH INTERNATIONAL WORKSHOP ON TROPICAL CYCLONES Topic 2: Cyclogenesis, Intensity and Intensity Change Topic chairs: Elizabeth A. Ritchie (UA) and Chun-Chieh Wu (NTU) Rapporteurs: Anantha Aiyyar (NCSU),

More information

Topic 2.2 CYCLOGENESIS: OPERATIONAL FORECASTING PERSPECTIVE

Topic 2.2 CYCLOGENESIS: OPERATIONAL FORECASTING PERSPECTIVE Topic 2.2 CYCLOGENESIS: OPERATIONAL FORECASTING PERSPECTIVE Rapporteur: Christopher W. Landsea National Hurricane Center RSMC Miami 11691 SW 17 th Street Miami, FL, 33165, U.S.A. Email: Chris.Landsea@noaa.gov

More information

TROPICAL CYCLONE GENESIS. Todd B. Kimberlain and Richard J. Pasch WMO RA-IV Workshop on Hurricane Forecasting & Warning 7 March 2016

TROPICAL CYCLONE GENESIS. Todd B. Kimberlain and Richard J. Pasch WMO RA-IV Workshop on Hurricane Forecasting & Warning 7 March 2016 TROPICAL CYCLONE GENESIS Todd B. Kimberlain and Richard J. Pasch WMO RA-IV Workshop on Hurricane Forecasting & Warning 7 March 2016 Outline / Topics Climatology Large-scale conditions associated with tropical

More information

Lectures on Tropical Cyclones

Lectures on Tropical Cyclones Lectures on Tropical Cyclones Chapter 1 Observations of Tropical Cyclones Outline of course Introduction, Observed Structure Dynamics of Mature Tropical Cyclones Equations of motion Primary circulation

More information

TROPICAL CYCLONE TC 03A FOR THE PERIOD 3 RD JUNE TO 10 TH JUNE, 1998

TROPICAL CYCLONE TC 03A FOR THE PERIOD 3 RD JUNE TO 10 TH JUNE, 1998 TROPICAL CYCLONE TC 03A FOR THE PERIOD 3 RD JUNE TO 10 TH JUNE, 1998 Hazrat Mir, Abdul Rashid, Waqarul Wheed Khan. Introduction: This report gives the review of cyclonic storm formed over the East Arabian

More information

Case Studies in Communication Challenges: Hurricane Sandy

Case Studies in Communication Challenges: Hurricane Sandy Case Studies in Communication Challenges: Hurricane Sandy International Workshop on Tropical Cyclones Jeju Island, South Korea Chris Landsea, National Hurricane Center, RSMC Miami Major Hurricane Sandy

More information

Subtropical and Hybrid Systems IWTC VII Topic 1.6

Subtropical and Hybrid Systems IWTC VII Topic 1.6 Subtropical and Hybrid Systems IWTC VII Topic 1.6 John R. Gyakum Department of Atmospheric and Oceanic Sciences McGill University, Montreal Canada Working group: John L. Beven II, Lance F. Bosart, Fermin

More information

Tropical Cyclone Genesis: What we know, and what we don t!

Tropical Cyclone Genesis: What we know, and what we don t! Tropical Cyclone Genesis: What we know, and what we don t! Allison Wing! NSF Postdoctoral Research Fellow! Lamont-Doherty Earth Observatory! Columbia University! Overview! Climatology! What We Know! Theories!

More information

(April 7, 2010, Wednesday) Tropical Storms & Hurricanes Part 2

(April 7, 2010, Wednesday) Tropical Storms & Hurricanes Part 2 Lecture #17 (April 7, 2010, Wednesday) Tropical Storms & Hurricanes Part 2 Hurricane Katrina August 2005 All tropical cyclone tracks (1945-2006). Hurricane Formation While moving westward, tropical disturbances

More information

SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES. Working Group: Phillipe Caroff, Jeff Callaghan, James Franklin, Mark DeMaria

SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES. Working Group: Phillipe Caroff, Jeff Callaghan, James Franklin, Mark DeMaria WMO/CAS/WWW Topic 0.1: Track forecasts SIXTH INTERNATIONAL WORKSHOP on TROPICAL CYCLONES Rapporteur: E-mail: Lixion A. Avila NOAA/National Hurricane Center 11691 SW 17th Street Miami, FL 33165-2149, USA

More information

Hurricanes and Tropical Weather Systems:

Hurricanes and Tropical Weather Systems: Hurricanes and Tropical Weather Systems: An influence on weather in parts of the USA Meteorology 411 Iowa State University Week 2 Bill Gallus Classification/Terminology Tropical Disturbance enhanced convection

More information

Hurricane Structure: Theory and Diagnosis

Hurricane Structure: Theory and Diagnosis Hurricane Structure: Theory and Diagnosis 7 March, 2016 World Meteorological Organization Workshop Chris Landsea Chris.Landsea@noaa.gov National Hurricane Center, Miami Outline Structure of Hurricanes

More information

ESCI 344 Tropical Meteorology Lesson 11 Tropical Cyclones: Formation, Maintenance, and Intensification

ESCI 344 Tropical Meteorology Lesson 11 Tropical Cyclones: Formation, Maintenance, and Intensification ESCI 344 Tropical Meteorology Lesson 11 Tropical Cyclones: Formation, Maintenance, and Intensification References: A Global View of Tropical Cyclones, Elsberry (ed.) Global Perspectives on Tropical Cylones:

More information

Aviation Hazards: Thunderstorms and Deep Convection

Aviation Hazards: Thunderstorms and Deep Convection Aviation Hazards: Thunderstorms and Deep Convection TREND NWP Products for Thunderstorm Forecasting Contents Model choice Identifying parameters important for convection: Low-level convergence High relative

More information

4. Climatic changes. Past variability Future evolution

4. Climatic changes. Past variability Future evolution 4. Climatic changes Past variability Future evolution TROPICAL CYCLONES and CLIMATE How TCs have varied during recent and distant past? How will TC activity vary in the future? 2 CURRENT CLIMATE : how

More information

Tropical Waves. John Cangialosi and Lixion Avila National Hurricane Center. WMO Region IV Tropical Cyclone Workshop

Tropical Waves. John Cangialosi and Lixion Avila National Hurricane Center. WMO Region IV Tropical Cyclone Workshop Tropical Waves John Cangialosi and Lixion Avila National Hurricane Center WMO Region IV Tropical Cyclone Workshop Outline Basic definition Schematic diagrams/interactions Operational products/forecasts

More information

NHC Ensemble/Probabilistic Guidance Products

NHC Ensemble/Probabilistic Guidance Products NHC Ensemble/Probabilistic Guidance Products Michael Brennan NOAA/NWS/NCEP/NHC Mark DeMaria NESDIS/STAR HFIP Ensemble Product Development Workshop 21 April 2010 Boulder, CO 1 Current Ensemble/Probability

More information

Examination of Tropical Cyclogenesis using the High Temporal and Spatial Resolution JRA-25 Dataset

Examination of Tropical Cyclogenesis using the High Temporal and Spatial Resolution JRA-25 Dataset Examination of Tropical Cyclogenesis using the High Temporal and Spatial Resolution JRA-25 Dataset Masato Sugi Forecast Research Department, Meteorological Research Institute, Japan Correspondence: msugi@mri-jma.go.jp

More information

AGENDA ITEM 2.1: OPERATIONAL FORECASTS/ADVISORIES, WATCHES AND WARNINGS - REQUIREMENTS

AGENDA ITEM 2.1: OPERATIONAL FORECASTS/ADVISORIES, WATCHES AND WARNINGS - REQUIREMENTS World Meteorological Organization TROPICAL CYCLONE RSMCS/TCWCS TECHNICAL COORDINATION MEETING Ninth Session Honolulu, Hawaii, USA, 9 to 12 December 2018 TCM-9/DOC.2.1.1/4 Submitted by: TCWC Wellington

More information

The Extratropical Transition of Tropical Cyclones

The Extratropical Transition of Tropical Cyclones The Extratropical Transition of Tropical Cyclones Elizabeth A. Ritchie Department of Electrical and Computer Engineering and the Center for High Performance Computing Room 125, EECE Building Albuquerque,

More information

ESCI 241 Meteorology Lesson 19 Tropical Cyclones Dr. DeCaria

ESCI 241 Meteorology Lesson 19 Tropical Cyclones Dr. DeCaria ESCI 241 Meteorology Lesson 19 Tropical Cyclones Dr. DeCaria READING: Chapter 16 GENERAL A tropical cyclone is a large, low-pressure system that forms over the tropical oceans. Tropical cyclones are classified

More information

Tropical Cyclone Formation/Structure/Motion Studies

Tropical Cyclone Formation/Structure/Motion Studies Tropical Cyclone Formation/Structure/Motion Studies Patrick A. Harr Department of Meteorology Naval Postgraduate School Monterey, CA 93943-5114 phone: (831) 656-3787 fax: (831) 656-3061 email: paharr@nps.edu

More information

Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas

Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas Prince K. Xavier and P.V. Joseph Department of Atmospheric Sciences Cochin University of Science

More information

Understanding the Global Distribution of Monsoon Depressions

Understanding the Global Distribution of Monsoon Depressions DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Understanding the Global Distribution of Monsoon Depressions William R. Boos PO Box 208109 New Haven, CT 06520 phone: (203)

More information

Hurricane Structure: Theory and Application. John Cangialosi National Hurricane Center

Hurricane Structure: Theory and Application. John Cangialosi National Hurricane Center Hurricane Structure: Theory and Application John Cangialosi National Hurricane Center World Meteorological Organization Workshop Is this Tropical, Subtropical, or Extratropical? Subtropical Tropical Extratropical

More information

Predicting Tropical Cyclone Formation and Structure Change

Predicting Tropical Cyclone Formation and Structure Change Predicting Tropical Cyclone Formation and Structure Change Patrick A. Harr Department of Meteorology Naval Postgraduate School Monterey, CA 93943-5114 phone: (831)656-3787 fax: (831)656-3061 email: paharr@nps.navy.mil

More information

Recent ET/STC/TT near Iberian Peninsula and Canary Islands

Recent ET/STC/TT near Iberian Peninsula and Canary Islands Recent ET/STC/TT near Iberian Peninsula and Canary Islands ET, Extratropical Transition STC, SubTropical Cyclogenesis TT, Tropical Transition Francisco Martín and Fermín Elizaga AEMet francisco.martín@inm.es

More information

1. INTRODUCTION: 2. DATA AND METHODOLOGY:

1. INTRODUCTION: 2. DATA AND METHODOLOGY: 27th Conference on Hurricanes and Tropical Meteorology, 24-28 April 2006, Monterey, CA 3A.4 SUPERTYPHOON DALE (1996): A REMARKABLE STORM FROM BIRTH THROUGH EXTRATROPICAL TRANSITION TO EXPLOSIVE REINTENSIFICATION

More information

Hurricanes Part I Structure and Climatology by Professor Steven Businger. Hurricane Katrina

Hurricanes Part I Structure and Climatology by Professor Steven Businger. Hurricane Katrina Hurricanes Part I Structure and Climatology by Professor Steven Businger Hurricane Katrina Hurricanes Part I Structure and Climatology by Professor Steven Businger What is a hurricane? What is the structure

More information

A Reformulation of the Logistic Growth Equation Model (LGEM) for Ensemble and Extended Range Intensity Prediction

A Reformulation of the Logistic Growth Equation Model (LGEM) for Ensemble and Extended Range Intensity Prediction A Reformulation of the Logistic Growth Equation Model (LGEM) for Ensemble and Extended Range Intensity Prediction Mark DeMaria NOAA/NESDIS, Fort Collins, CO Andrea Schumacher and Kate Musgrave CIRA/CSU,

More information

Tropical Cyclones: When Nature Attacks!! AOSC 200 Tim Canty. Tropical Cyclone: African Easterly Jet

Tropical Cyclones: When Nature Attacks!! AOSC 200 Tim Canty. Tropical Cyclone: African Easterly Jet Tropical Cyclones: When Nature Attacks!! AOSC 200 Tim Canty Class Web Site: http://www.atmos.umd.edu/~tcanty/aosc200 Topics for today: Really powerful low pressure systems Lecture 25 Nov 27 2018 1 Tropical

More information

Tropical Cyclone Intensity and Structure Changes due to Upper-Level Outflow and Environmental Interactions

Tropical Cyclone Intensity and Structure Changes due to Upper-Level Outflow and Environmental Interactions DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Tropical Cyclone Intensity and Structure Changes due to Upper-Level Outflow and Environmental Interactions Russell L. Elsberry

More information

Tropical Cyclones. Objectives

Tropical Cyclones. Objectives Tropical Cyclones FIU Undergraduate Hurricane Internship Lecture 2 8/8/2012 Objectives From this lecture you should understand: Global tracks of TCs and the seasons when they are most common General circulation

More information

11/19/14. Chapter 11: Hurricanes. The Atmosphere: An Introduction to Meteorology, 12 th. Lutgens Tarbuck

11/19/14. Chapter 11: Hurricanes. The Atmosphere: An Introduction to Meteorology, 12 th. Lutgens Tarbuck Chapter 11: Hurricanes The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University! Hurricanes: " Hurricanes are intense centers of

More information

Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan

Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan 10A.4 TROPICAL CYCLONE FORMATIONS IN THE SOUTH CHINA SEA CHENG-SHANG LEE 1 AND YUNG-LAN LIN* 1, 2 1 Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan 2 Taipei Aeronautic Meteorological

More information

Extratropical transition of tropical cyclones: Operational forecasting challenges. Matthew Kucas Joint Typhoon Warning Center Pearl Harbor, HI, USA

Extratropical transition of tropical cyclones: Operational forecasting challenges. Matthew Kucas Joint Typhoon Warning Center Pearl Harbor, HI, USA Extratropical transition of tropical cyclones: Operational forecasting challenges Matthew Kucas Joint Typhoon Warning Center Pearl Harbor, HI, USA Outline Motivation for discussion Brief overview of tropical

More information

1. INTRODUCTION. designed. The primary focus of this strategy was the extratropical transition (ET) of tropical cyclones based on the poleward

1. INTRODUCTION. designed. The primary focus of this strategy was the extratropical transition (ET) of tropical cyclones based on the poleward P1.98 THE THORPEX PACIFIC ASIAN REGIONAL CAMPAIGN (T-PARC) OBJECTIVE ON THE EXTRATROPICAL TRANSITION OF TROPICAL CYCLONES: OBSERVED CASES, THEIR STRUCTURE AND DOWNSTREAM IMPACTS P. A. Harr 1, S. C. Jones

More information

- Introduction - Technical Presentation 49 th Session of the Typhoon Committee. Yokohama, Japan 21 February Munehiko Yamaguchi

- Introduction - Technical Presentation 49 th Session of the Typhoon Committee. Yokohama, Japan 21 February Munehiko Yamaguchi - Introduction - The Latest Model Simulation and Observational Studies related to Tropical Cyclone in Japan Technical Presentation 49 th Session of the Typhoon Committee Yokohama, Japan 21 February 2017

More information

On African easterly waves that impacted two tropical cyclones in 2004

On African easterly waves that impacted two tropical cyclones in 2004 GEOPHYSICAL RESEARCH LETTERS, VOL. 33,, doi:10.1029/2006gl026038, 2006 On African easterly waves that impacted two tropical cyclones in 2004 Melinda S. Peng, 1 Bing Fu, 2 Timothy F. Hogan, 1 and Tim Li

More information

Have a better understanding of the Tropical Cyclone Products generated at ECMWF

Have a better understanding of the Tropical Cyclone Products generated at ECMWF Objectives Have a better understanding of the Tropical Cyclone Products generated at ECMWF Learn about the recent developments in the forecast system and its impact on the Tropical Cyclone forecast Learn

More information

The Impact of air-sea interaction on the extratropical transition of tropical cyclones

The Impact of air-sea interaction on the extratropical transition of tropical cyclones The Impact of air-sea interaction on the extratropical transition of tropical cyclones Sarah Jones Institut für Meteorologie und Klimaforschung Universität Karlsruhe / Forschungszentrum Karlsruhe 1. Introduction

More information

- tornadoes. Further Reading: Chapter 08 of the text book. Outline. -tropical storms. -Storm surge

- tornadoes. Further Reading: Chapter 08 of the text book. Outline. -tropical storms. -Storm surge (1 of 12) Further Reading: Chapter 08 of the text book Outline - tornadoes -tropical storms -Storm surge (2 of 12) Introduction Previously, We talked about fronts and their relationship to air masses Also

More information

Ensemble Prediction Systems

Ensemble Prediction Systems Ensemble Prediction Systems Eric Blake National Hurricane Center 7 March 2017 Acknowledgements to Michael Brennan 1 Question 1 What are some current advantages of using single-model ensembles? A. Estimates

More information

Multiscale Analyses of Inland Tropical Cyclone Midlatitude Jet Interactions: Camille (1969) and Danny (1997)

Multiscale Analyses of Inland Tropical Cyclone Midlatitude Jet Interactions: Camille (1969) and Danny (1997) Multiscale Analyses of Inland Tropical Cyclone Midlatitude Jet Interactions: Camille (1969) and Danny (1997) Matthew Potter, Lance Bosart, and Daniel Keyser Department of Atmospheric and Environmental

More information

Scale Interactions during the Formation of Typhoon Irving 边建谱 ELIZABETH A. RITCHIE GREG J. HOLLAND

Scale Interactions during the Formation of Typhoon Irving 边建谱 ELIZABETH A. RITCHIE GREG J. HOLLAND Scale Interactions during the Formation of Typhoon Irving 边建谱 ELIZABETH A. RITCHIE GREG J. HOLLAND Pre-research Fujiwhara: laboratory experiments in water (1921, 1923, 1931). Cloud clusters are a well-known

More information

Annual Number of Peer Reviewed Articles with Hurricane or Tropical Cyclone in their Titles, according to Meteorological and Geoastrophysical

Annual Number of Peer Reviewed Articles with Hurricane or Tropical Cyclone in their Titles, according to Meteorological and Geoastrophysical Hurricanes and Climate Kerry Emanuel Program in Atmospheres, Oceans, and Climate MIT Program Potential Intensity Role of potential ti li intensity it in storm intensity it Role of potential intensity in

More information

T-PARC and TCS08 (Submitted by Pat Harr, Russell Elsberry and Tetsuo Nakazawa)

T-PARC and TCS08 (Submitted by Pat Harr, Russell Elsberry and Tetsuo Nakazawa) WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR ATMOSPHERIC SCIENCES INTERNATIONAL CORE STEERING COMMITTEE FOR THORPEX Eighth Session DWD, Offenbach (2 4 November 2009) CAS/ICSC-8/DOC4.1 (3 X.2009) Item:

More information

JMA Contribution to SWFDDP in RAV. (Submitted by Yuki Honda and Masayuki Kyouda, Japan Meteorological Agency) Summary and purpose of document

JMA Contribution to SWFDDP in RAV. (Submitted by Yuki Honda and Masayuki Kyouda, Japan Meteorological Agency) Summary and purpose of document WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR BASIC SYSTEMS OPAG on DPFS DPFS/RAV-SWFDDP-RSMT Doc. 7.1(1) (28.X.2010) SEVERE WEATHER FORECASTING AND DISASTER RISK REDUCTION DEMONSTRATION PROJECT (SWFDDP)

More information

Storm Summary for Hurricane Jose

Storm Summary for Hurricane Jose Storm Summary for Hurricane Jose Tuesday, September 19, 2017 at 11 AM EDT (Output from Hurrevac, based on National Hurricane Center Forecast Advisory #57) Jose is currently a Category 1 hurricane on the

More information

Chapter 24 Tropical Cyclones

Chapter 24 Tropical Cyclones Chapter 24 Tropical Cyclones Tropical Weather Systems Tropical disturbance a cluster of thunderstorms about 250 to 600 km in diameter, originating in the tropics or sub-tropics Tropical depression a cluster

More information

COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL CYCLONE PROGRAMME

COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL CYCLONE PROGRAMME ESCAP/WMO Typhoon Committee The Fifty-First Session 26 Feb 1 Mar 2019 Guangzhou, China FOR PARTICIPANTS ONLY WRD/TC.51/14 24 February 2019 ENGLISH ONLY COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL

More information

A Preliminary Climatology of Extratropical Transitions in the Southwest Indian Ocean

A Preliminary Climatology of Extratropical Transitions in the Southwest Indian Ocean A Preliminary Climatology of Extratropical Transitions in the Southwest Indian Ocean Kyle S. Griffin Department of Atmospheric and Environmental Sciences, University at Albany, State University of New

More information

Tropical-Extratropical Transition

Tropical-Extratropical Transition Tropical-Extratropical Transition Extratropical Transition A significant number of tropical cyclones move into the midlatitudes and transform into extratropical cyclones. This process is generally referred

More information

TROPICAL CYCLONE GENESIS IN TC-LAPS: THE IMPORTANCE OF SUFFICIENT NET DEEP CONVECTION AND SYSTEM SCALE CYCLONIC ABSOLUTE VORTICITY

TROPICAL CYCLONE GENESIS IN TC-LAPS: THE IMPORTANCE OF SUFFICIENT NET DEEP CONVECTION AND SYSTEM SCALE CYCLONIC ABSOLUTE VORTICITY 14A.1 TROPICAL CYCLONE GENESIS IN TC-LAPS: THE IMPORTANCE OF SUFFICIENT NET DEEP CONVECTION AND SYSTEM SCALE CYCLONIC ABSOLUTE VORTICITY Kevin J. Tory 1, Noel E. Davidson Bureau of Meteorology Research

More information

The 2009 Hurricane Season Overview

The 2009 Hurricane Season Overview The 2009 Hurricane Season Overview Jae-Kyung Schemm Gerry Bell Climate Prediction Center NOAA/ NWS/ NCEP 1 Overview outline 1. Current status for the Atlantic, Eastern Pacific and Western Pacific basins

More information

Introduction forecast Procedure of National Typhoon Center / KMA

Introduction forecast Procedure of National Typhoon Center / KMA The 6 th China-Korea Joint Workshop on Tropical Cyclones (26 May-1 June, 2013) Introduction forecast Procedure of National Typhoon Center / KMA Lee, Jae-shin(jaeshin_l@yahoo.com) National Typhoon Center(NTC)

More information

PRMS WHITE PAPER 2014 NORTH ATLANTIC HURRICANE SEASON OUTLOOK. June RMS Event Response

PRMS WHITE PAPER 2014 NORTH ATLANTIC HURRICANE SEASON OUTLOOK. June RMS Event Response PRMS WHITE PAPER 2014 NORTH ATLANTIC HURRICANE SEASON OUTLOOK June 2014 - RMS Event Response 2014 SEASON OUTLOOK The 2013 North Atlantic hurricane season saw the fewest hurricanes in the Atlantic Basin

More information

Recent Developments of JMA Operational NWP Systems and WGNE Intercomparison of Tropical Cyclone Track Forecast

Recent Developments of JMA Operational NWP Systems and WGNE Intercomparison of Tropical Cyclone Track Forecast Recent Developments of JMA Operational NWP Systems and WGNE Intercomparison of Tropical Cyclone Track Forecast Chiashi Muroi Numerical Prediction Division Japan Meteorological Agency 1 CURRENT STATUS AND

More information

WMO. Early Warning System

WMO. Early Warning System World Meteorological Organization Working together in weather, climate and water WMO Tropical Cyclone Early Warning System Koji Kuroiwa Tropical Cyclone Programme World Meteorological Organization For

More information

Impact of GPS RO Data on the Prediction of Tropical Cyclones

Impact of GPS RO Data on the Prediction of Tropical Cyclones Impact of GPS RO Data on the Prediction of Tropical Cyclones Ying-Hwa Kuo, Hui Liu, UCAR Ching-Yuang Huang, Shu-Ya Chen, NCU Ling-Feng Hsiao, Ming-En Shieh, Yu-Chun Chen, TTFRI Outline Tropical cyclone

More information

Understanding the Global Distribution of Monsoon Depressions

Understanding the Global Distribution of Monsoon Depressions DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Understanding the Global Distribution of Monsoon Depressions William R. Boos PO Box 208109 New Haven, CT 06520 phone: (203)

More information

Transient/Eddy Flux. Transient and Eddy. Flux Components. Lecture 7: Disturbance (Outline) Why transients/eddies matter to zonal and time means?

Transient/Eddy Flux. Transient and Eddy. Flux Components. Lecture 7: Disturbance (Outline) Why transients/eddies matter to zonal and time means? Lecture 7: Disturbance (Outline) Transients and Eddies Climate Roles Mid-Latitude Cyclones Tropical Hurricanes Mid-Ocean Eddies (From Weather & Climate) Flux Components (1) (2) (3) Three components contribute

More information

Impact of Stochastic Convection on Ensemble Forecasts of Tropical Cyclone Development

Impact of Stochastic Convection on Ensemble Forecasts of Tropical Cyclone Development 620 M O N T H L Y W E A T H E R R E V I E W VOLUME 139 Impact of Stochastic Convection on Ensemble Forecasts of Tropical Cyclone Development ANDREW SNYDER AND ZHAOXIA PU Department of Atmospheric Sciences,

More information

COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL CYCLONE PROGRAMME. (Submitted by the WMO Secretariat) Summary and Purpose of Document

COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL CYCLONE PROGRAMME. (Submitted by the WMO Secretariat) Summary and Purpose of Document ESCAP/WMO TYPHOON COMMITTEE FORTY-NINTH SESSION 21-24 FEBRUARY 2017 YOKOHAMA, JAPAN FOR PARTICIPANTS ONLY WRD/TC.49/16 13 February 2017 ENGLISH ONLY COORDINATION WITH OTHER ACTIVITIES OF THE WMO TROPICAL

More information

CHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS

CHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS CHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS 1. Viewed from above in the Northern Hemisphere, surface winds about a subtropical high blow a. clockwise and inward. b. counterclockwise.

More information

Hurricanes. April 14, 2009

Hurricanes. April 14, 2009 Tropical Weather & Hurricanes Chapter 15 April 14, 2009 Tropical meteorology Tropics characterized by seasonal wet and drier periods- wet when sun is nearly overhead at noon and inter-tropical convergence

More information

Predicting Tropical Cyclone Genesis

Predicting Tropical Cyclone Genesis DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Predicting Tropical Cyclone Genesis PI: Melinda S. Peng Naval Research Laboratory Monterey CA 93943-5502 Phone: (831) 656-4704

More information

Lecture 18 Hurricanes

Lecture 18 Hurricanes Lecture 18 Hurricanes Part I Structure and Climatology What is a hurricane? What is the structure or anatomy of a hurricane? How to build a hurricane - hurricane energy Hurricane climatology - when and

More information

Transient and Eddy. Transient/Eddy Flux. Flux Components. Lecture 3: Weather/Disturbance. Transient: deviations from time mean Time Mean

Transient and Eddy. Transient/Eddy Flux. Flux Components. Lecture 3: Weather/Disturbance. Transient: deviations from time mean Time Mean Lecture 3: Weather/Disturbance Transients and Eddies Climate Roles Mid-Latitude Cyclones Tropical Hurricanes Mid-Ocean Eddies Transient and Eddy Transient: deviations from time mean Time Mean Eddy: deviations

More information

Comments on: Increasing destructiveness of tropical cyclones over the past 30 years by Kerry Emanuel, Nature, 31 July 2005, Vol. 436, pp.

Comments on: Increasing destructiveness of tropical cyclones over the past 30 years by Kerry Emanuel, Nature, 31 July 2005, Vol. 436, pp. Comments on: Increasing destructiveness of tropical cyclones over the past 30 years by Kerry Emanuel, Nature, 31 July 2005, Vol. 436, pp. 686-688 William M. Gray Department of Atmospheric Science Colorado

More information

The Pressure s On: Increased. Introduction. By Jason Butke Edited by Meagan Phelan

The Pressure s On: Increased. Introduction. By Jason Butke Edited by Meagan Phelan The Pressure s On: Increased Realism in Tropical Cyclone Wind Speeds through Attention to Environmental Pressure 01.2012 By Jason Butke Introduction Because the Earth has a tilted axis and rotates, the

More information

16 th RAV/TCC Meeting, Solomon Is Misaeli Funaki- RSMC Nadi

16 th RAV/TCC Meeting, Solomon Is Misaeli Funaki- RSMC Nadi 16 th RAV/TCC Meeting, Solomon Is. 2016 Misaeli Funaki- RSMC Nadi 2014/15 seasonal activities reviewed -Climate Indices - MJO..etc - Seasonal Review 2015/16 seasonal activities reviewed -Climate Indices

More information

Critical Thinking Review

Critical Thinking Review Critical Thinking Review (wk3) Cognitive Skill of the Week: Analysis Analysis is the examination of a system (or complex), its components (or ingredients), and the linkages among these components. One

More information

NHC Ocean Vector Winds Update

NHC Ocean Vector Winds Update NHC Ocean Vector Winds Update Michael J. Brennan NOAA/NWS/NCEP National Hurricane Center International Ocean Vector Winds Science Team Meeting Portland, Oregon, 20 May 2015 Current Status NHC is currently

More information

Fernando Prates. Evaluation Section. Slide 1

Fernando Prates. Evaluation Section. Slide 1 Fernando Prates Evaluation Section Slide 1 Objectives Ø Have a better understanding of the Tropical Cyclone Products generated at ECMWF Ø Learn the recent developments in the forecast system and its impact

More information

QUADRENNIAL WORKSHOP PREVIEW

QUADRENNIAL WORKSHOP PREVIEW QUADRENNIAL WORKSHOP PREVIEW BACKGROUND The International Workshop on Tropical Cyclones (IWTC) was conceived in the early 1980 s by a small group of tropical cyclone meteorologists led by Professor William

More information

Observed Structure and Environment of Developing and Nondeveloping Tropical Cyclones in the Western North Pacific using Satellite Data

Observed Structure and Environment of Developing and Nondeveloping Tropical Cyclones in the Western North Pacific using Satellite Data DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Observed Structure and Environment of Developing and Nondeveloping Tropical Cyclones in the Western North Pacific using

More information

Assessing Land Surface Albedo Bias in Models of Tropical Climate

Assessing Land Surface Albedo Bias in Models of Tropical Climate DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Assessing Land Surface Albedo Bias in Models of Tropical Climate William R. Boos (PI) Yale University PO Box 208109 New

More information

GFDL Hurricane Model Ensemble Performance During the 2012 Hurricane Season

GFDL Hurricane Model Ensemble Performance During the 2012 Hurricane Season GFDL Hurricane Model Ensemble Performance During the 2012 Hurricane Season Tim Marchok (NOAA / GFDL) Matt Morin (DRC HPTG / GFDL) Morris Bender (NOAA / GFDL) HFIP Team Telecon 12 December 2012 Acknowledgments:

More information

- tornadoes. Further Reading: Chapter 08 of the text book. Outline. - cyclones and anti-cyclones. -tropical storms. -Storm surge

- tornadoes. Further Reading: Chapter 08 of the text book. Outline. - cyclones and anti-cyclones. -tropical storms. -Storm surge (1 of 16) Further Reading: Chapter 08 of the text book Outline - cyclones and anti-cyclones - tornadoes -tropical storms -Storm surge (2 of 16) Introduction Previously, We talked about fronts and their

More information

Lec 10: Interpreting Weather Maps

Lec 10: Interpreting Weather Maps Lec 10: Interpreting Weather Maps Case Study: October 2011 Nor easter FIU MET 3502 Synoptic Hurricane Forecasts Genesis: on large scale weather maps or satellite images, look for tropical waves (Africa

More information

Why There Is Weather?

Why There Is Weather? Lecture 6: Weather, Music Of Our Sphere Weather and Climate WEATHER The daily fluctuations in atmospheric conditions. The atmosphere on its own can produce weather. (From Understanding Weather & Climate)

More information

Motivation & Goal. We investigate a way to generate PDFs from a single deterministic run

Motivation & Goal. We investigate a way to generate PDFs from a single deterministic run Motivation & Goal Numerical weather prediction is limited by errors in initial conditions, model imperfections, and nonlinearity. Ensembles of an NWP model provide forecast probability density functions

More information

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS 1. The atmosphere is a continuous fluid that envelops the globe, so that weather observation, analysis, and forecasting require international

More information

CPTEC and NCEP Model Forecast Drift and South America during the Southern Hemisphere Summer

CPTEC and NCEP Model Forecast Drift and South America during the Southern Hemisphere Summer CPTEC and NCEP Model Forecast Drift and South America during the Southern Hemisphere Summer José Antonio Aravéquia 1 Pedro L. Silva Dias 2 (1) Center for Weather Forecasting and Climate Research National

More information

Predicting Tropical Cyclone Formation and Structure Change

Predicting Tropical Cyclone Formation and Structure Change Predicting Tropical Cyclone Formation and Structure Change Patrick A. Harr Department of Meteorology Naval Postgraduate School Monterey, CA 93943-5114 Telephone: (831)656-3787 FAX:(831)656-3061 email:

More information

Objectives for meeting

Objectives for meeting Objectives for meeting 1) Summarize planned experiments 2) Discuss resource availability Aircraft Instrumentation Expendables 3) Assign working groups to complete each experiment plan Flight planning and

More information

2) What general circulation wind belt is the place of origin for hurricanes? A) westerlies B) trade winds C) doldrums D) horse latitudes

2) What general circulation wind belt is the place of origin for hurricanes? A) westerlies B) trade winds C) doldrums D) horse latitudes Meteo 1010 Homework 6 1) What is the difference between a typhoon and a hurricane? A) A hurricane is a true tropical cyclone, but a typhoon is not. B) A hurricane is stronger than a typhoon. C) They represent

More information

Recent advances in Tropical Cyclone prediction using ensembles

Recent advances in Tropical Cyclone prediction using ensembles Recent advances in Tropical Cyclone prediction using ensembles Richard Swinbank, with thanks to Many colleagues in Met Office, GIFS-TIGGE WG & others HC-35 meeting, Curacao, April 2013 Recent advances

More information

August Forecast Update for Atlantic Hurricane Activity in 2012

August Forecast Update for Atlantic Hurricane Activity in 2012 August Forecast Update for Atlantic Hurricane Activity in 2012 Issued: 6 th August 2012 by Professor Mark Saunders and Dr Adam Lea Dept. of Space and Climate Physics, UCL (University College London), UK

More information

Characteristics of Sudden Changes in Tropical Cyclone Tracks over North Indian Ocean. M. Mohapatra and B. K. Bandyopadhyay

Characteristics of Sudden Changes in Tropical Cyclone Tracks over North Indian Ocean. M. Mohapatra and B. K. Bandyopadhyay Characteristics of Sudden Changes in Tropical Cyclone Tracks over North Indian Ocean M. Mohapatra and B. K. Bandyopadhyay INDIA METEOROLOGICAL DEPARTMENT MAUSAM BHAVAN, LODI ROAD, NEW DELHI 110003 mohapatraimd@gmail.com

More information

SH RI Events. Influence From Patterns Of Different Scale

SH RI Events. Influence From Patterns Of Different Scale SH072014 RI Events Influence From Patterns Of Different Scale RI Explanation * Rapid intensification, approximately an increase of 2 Dvorak T-numbers or 30 knots in 24 hours, frequently occurs in JTWC

More information

10B.2 THE ROLE OF THE OCCLUSION PROCESS IN THE EXTRATROPICAL-TO-TROPICAL TRANSITION OF ATLANTIC HURRICANE KAREN

10B.2 THE ROLE OF THE OCCLUSION PROCESS IN THE EXTRATROPICAL-TO-TROPICAL TRANSITION OF ATLANTIC HURRICANE KAREN 10B.2 THE ROLE OF THE OCCLUSION PROCESS IN THE EXTRATROPICAL-TO-TROPICAL TRANSITION OF ATLANTIC HURRICANE KAREN Andrew L. Hulme* and Jonathan E. Martin University of Wisconsin-Madison, Madison, Wisconsin

More information

and 24 mm, hPa lapse rates between 3 and 4 K km 1, lifted index values

and 24 mm, hPa lapse rates between 3 and 4 K km 1, lifted index values 3.2 Composite analysis 3.2.1 Pure gradient composites The composite initial NE report in the pure gradient northwest composite (N = 32) occurs where the mean sea level pressure (MSLP) gradient is strongest

More information

Development of JMA storm surge model

Development of JMA storm surge model 2 nd JCOMM Scientific and Technical Symposium on Storm Surges 8-13 November 2015, Key West, Florida, USA Development of JMA storm surge model Hiroshi HASEGAWA (h_hasegawa@met.kishou.go.jp) Office of Marine

More information

Chapter 24. Tropical Cyclones. Tropical Cyclone Classification 4/19/17

Chapter 24. Tropical Cyclones. Tropical Cyclone Classification 4/19/17 Chapter 24 Tropical Cyclones Tropical Cyclones Most destructive storms on the planet Originate over tropical waters, but their paths often take them over land and into midlatitudes Names Hurricane (Atlantic

More information

Upgrade of JMA s Typhoon Ensemble Prediction System

Upgrade of JMA s Typhoon Ensemble Prediction System Upgrade of JMA s Typhoon Ensemble Prediction System Masayuki Kyouda Numerical Prediction Division, Japan Meteorological Agency and Masakazu Higaki Office of Marine Prediction, Japan Meteorological Agency

More information

Issued by the: Climate Services Division Fiji Meteorological Service Nadi Airport. 27 October 2010 GENERAL STATEMENT

Issued by the: Climate Services Division Fiji Meteorological Service Nadi Airport. 27 October 2010 GENERAL STATEMENT Fiji Meteorological Service (FMS) Tropical Cyclone Guidance for Season 2010/11 for the Fiji and the Southwest Pacific RSMC Region 160E to 120W Equator to 25 South Issued by the: Climate Services Division

More information

6. Changements Climatiques. Variabilité passée Evolution future

6. Changements Climatiques. Variabilité passée Evolution future 6. Changements Climatiques Variabilité passée Evolution future Tropical cyclone and climate change How TCs have varied during the instrumental record? How will TC activity vary in the future? Current Climate

More information

Developing versus Nondeveloping Disturbances for Tropical Cyclone Formation. Part II: Western North Pacific*

Developing versus Nondeveloping Disturbances for Tropical Cyclone Formation. Part II: Western North Pacific* APRIL 2012 F U E T A L. 1067 Developing versus Nondeveloping Disturbances for Tropical Cyclone Formation. Part II: Western North Pacific* BING FU International Pacific Research Center, University of Hawaii

More information