Downslope windstorm in High Tatras 19 November high resolution study by André Simon, Jozef Vivoda SHMÚ

Parametrization of convective gusts

from Newsletter Number 9 Spring 09 METEOROLOGY Parametrization of convective gusts doi:0.297/kfr42kfp8c This article appeared in the Meteorology section of ECMWF Newsletter No. 9 Spring 09, pp. -8. Parametrization

Climatological analysis of windstorm from November 2004 and evaluation of its impacts on meso- and microclimatic conditions in the High Tatras Region

Landform Analysis, Vol. 10: 108 114 (2009) Climatological analysis of windstorm from November 2004 and evaluation of its impacts on meso- and microclimatic conditions in the High Tatras Region Jozef Pecho*

Martin Benko *, Marián Jurašek, Ján Ka ák, André Simon, Jozef Vivoda Slovak Hydrometeorological Institute, SHMÚ, Slovak Republic

7.6 DEVELOPMENT OF NOWCASTING TECHNIQUES AT SHMÚ Martin Benko *, Marián Jurašek, Ján Ka ák, André Simon, Jozef Vivoda Slovak Hydrometeorological Institute, SHMÚ, Slovak Republic 1. INTRODUCTION Early attempts

Occlusion cyclogenesis II

Occlusion cyclogenesis II Upper level influences on cyclogenesis Vorticity Advection (CVA) and the 4-quadrant jet streak model (Uccellini) Potential Vorticity (PV) (Hoskins Theory) Rapid cyclogenesis 14

ALADIN forecast experience in Croatia

ALADIN forecast experience in Croatia Lidija Fustar and Tomislav Kozaric Meteorological and Hydrological Service ALADIN at DHMZ main source for the operational forecast at National Service of Croatia (along

Appalachian Lee Troughs and their Association with Severe Thunderstorms

Appalachian Lee Troughs and their Association with Severe Thunderstorms Daniel B. Thompson, Lance F. Bosart and Daniel Keyser Department of Atmospheric and Environmental Sciences University at Albany/SUNY,

Introduction to Mesoscale Meteorology

Introduction to Mesoscale Meteorology Overview Scale Definitions Synoptic Synoptic derived from Greek synoptikos meaning general view of the whole. Also has grown to imply at the same time or simultaneous.

CASE STUDY OF THE NOVEMBER WINDSTORM IN SOUTH CENTRAL COLORADO

32 CASE STUDY OF THE 12-13 NOVEMBER WINDSTORM IN SOUTH CENTRAL COLORADO Paul Wolyn * NOAA/NWS Pueblo, CO 1. INTRODUCTION During the evening and early morning of 12-13 November 2011, a damaging downslope

For the operational forecaster one important precondition for the diagnosis and prediction of

Initiation of Deep Moist Convection at WV-Boundaries Vienna, Austria For the operational forecaster one important precondition for the diagnosis and prediction of convective activity is the availability

High-resolution dynamical adaptation of the wind forecast using the non-hydrostatic version of the ALADIN model

High-resolution dynamical adaptation of the wind forecast using the non-hydrostatic version of the ALADIN model Steluta ALEXANDRU National Meteorological Administration, Bucharest, Romania steluta.alexandru@meteo.inmh.ro

1 August 2006 An Investigation of a Bow Echo along the Wasatch Front. Randy Graham and Chris Gibson 6 April 2007

1 August 2006 An Investigation of a Bow Echo along the Wasatch Front Randy Graham and Chris Gibson 6 April 2007 Overview Environment review Review of terrain-induced discrete propagation Bow Echo interactions

A Climatology of Windstorms in the Western Pacific Northwest,

A Climatology of Windstorms in the Western Pacific Northwest, 1948-2004 Wolf Read Oregon Climate Service College of Oceanic and Atmospheric Sciences Oregon State University Research Goals Compile data

THE LOW-LEVEL JET FOR BUCHAREST S AIRPORTS - A STUDY OF ITS CHARACTERISTICS IN WINTER SEASON BETWEEN 1959 AND 1982

Romanian Reports in Physics, Vol. 67. No. 2, P. 638 652, 2015 THE LOW-LEVEL JET FOR BUCHAREST S AIRPORTS - A STUDY OF ITS CHARACTERISTICS IN WINTER SEASON BETWEEN 1959 AND 1982 M. BALMEZ 1,2, F. GEORGESCU

Class exercises Chapter 3. Elementary Applications of the Basic Equations

Class exercises Chapter 3. Elementary Applications of the Basic Equations Section 3.1 Basic Equations in Isobaric Coordinates 3.1 For some (in fact many) applications we assume that the change of the Coriolis

Diabatic processes and the structure of extratropical cyclones

Geophysical and Nonlinear Fluid Dynamics Seminar AOPP, Oxford, 23 October 2012 Diabatic processes and the structure of extratropical cyclones Oscar Martínez-Alvarado R. Plant, J. Chagnon, S. Gray, J. Methven

Diabatic processes and the structure of the warm conveyor belt

2 nd European Windstorm Workshop Leeds, 3-4 September 2012 Diabatic processes and the structure of the warm conveyor belt Oscar Martínez-Alvarado J. Chagnon, S. Gray, R. Plant, J. Methven Department of

Inflow and Outflow through the Sea-to-Sky Corridor in February 2010: Lessons Learned from SNOW-V10 *

Inflow and Outflow through the Sea-to-Sky Corridor in February 2010: Lessons Learned from SNOW-V10 * Ruping Mo National Laboratory for Coastal and Mountain Meteorology, Environment Canada, Vancouver, BC,

Downscaling** a reanalysis for July 1996 "Big Freeze" in Southern NZ

Downscaling** a reanalysis for July 1996 "Big Freeze" in Southern NZ 2200 km* * Sydney to Auckland **with NOAA/NWS Sci. & Training Resource Center (STRC) "Environmental Modeling System" (EMS): WRF-ARW

Fronts in November 1998 Storm

Fronts in November 1998 Storm Much of the significant weather observed in association with extratropical storms tends to be concentrated within narrow bands called frontal zones. Fronts in November 1998

Nerushev A.F., Barkhatov A.E. Research and Production Association "Typhoon" 4 Pobedy Street, , Obninsk, Kaluga Region, Russia.

DETERMINATION OF ATMOSPHERIC CHARACTERISTICS IN THE ZONE OF ACTION OF EXTRA-TROPICAL CYCLONE XYNTHIA (FEBRUARY 2010) INFERRED FROM SATELLITE MEASUREMENT DATA Nerushev A.F., Barkhatov A.E. Research and

THE MESOSCALE CONVECTIVE SYSTEM FROM

RISCURI I CATASTROFE, NR.X, VOL.9, NR. 1/2011 THE MESOSCALE CONVECTIVE SYSTEM FROM 24.07.2010 ELZA HAUER, 1 C. NICHITA 1 ABSTRACT. The Mesoscale Convective System from 24.07.2010. A severe weather event

MAP Re-Analysis with IFS/ARPEGE/ALADIN

MAP Re-Analysis with IFS/ARPEGE/ALADIN Stjepan Ivatek-Šahdan RC LACE Data Manager Croatian Meteorological and Hydrological Service ivateks@cirus.dhz.hr Contents - Why to care about MAP-SOP Period? - Modification

Application and verification of ECMWF products 2012

Application and verification of ECMWF products 2012 Instituto Português do Mar e da Atmosfera, I.P. (IPMA) 1. Summary of major highlights ECMWF products are used as the main source of data for operational

p = ρrt p = ρr d = T( q v ) dp dz = ρg

Chapter 1: Properties of the Atmosphere What are the major chemical components of the atmosphere? Atmospheric Layers and their major characteristics: Troposphere, Stratosphere Mesosphere, Thermosphere

Severe Freezing Rain in Slovenia

Severe Freezing Rain in Slovenia Janez Markosek, Environmental Agency, Slovenia Introduction At the end of January and at the beginning of February 2014, severe and long-lasting freezing rain affected

Application and verification of ECMWF products 2016

Application and verification of ECMWF products 2016 RHMS of Serbia 1 Summary of major highlights ECMWF forecast products became the backbone in operational work during last several years. Starting from

High Resolution Numerical Modelling of a distinct extreme weather Cold Surges near Hong Kong region

High Resolution Numerical Modelling of a distinct extreme weather Cold Surges near Hong Kong region Anupam Kumar, Edmond Lo and Adam Switzer Email: aeroanupam@yahoo.co.in; anupam002@ntu.edu.sg Nanyang

Quasi-Geostrophic Implications

Chapter 10 Quasi-Geostrophic Implications When you look at a weather chart with all its isolines and plotted data, you need a framework upon which to interpret what you see. Quasi-geostrophic theory provides

Simon Tschannett*, B. Bica, B. Chimani, M. Dorninger, W. Gepp, S. Schneider, R. Steinacker University of Vienna Vienna, Austria

7.31 VERA AS AN OPERATIONAL NOWCASTING TOOL Simon Tschannett*, B. Bica, B. Chimani, M. Dorninger, W. Gepp, S. Schneider, R. Steinacker University of Vienna Vienna, Austria M. Kerschbaum Austro Control,

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

Mesoscale analysis of a comma cloud observed during FASTEX

Meteorol. Appl. 7, 129 134 (2000) Mesoscale analysis of a comma cloud observed during FASTEX K D Williams, Joint Centre for Mesoscale Meteorology, Department of Meteorology, University of Reading, PO Box

The Predictability of Extratropical Storm Tracks and the. Sensitivity of their Prediction to the Observing System

The Predictability of Extratropical Storm Tracks and the Sensitivity of their Prediction to the Observing System Lizzie S. R. Froude *, Lennart Bengtsson and Kevin I. Hodges Environmental Systems Science

Mesoscale meteorological models. Claire L. Vincent, Caroline Draxl and Joakim R. Nielsen

Mesoscale meteorological models Claire L. Vincent, Caroline Draxl and Joakim R. Nielsen Outline Mesoscale and synoptic scale meteorology Meteorological models Dynamics Parametrizations and interactions

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

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

Climatology of dry air intrusions and their relation to strong surface winds in extratropical cyclones

Climatology of dry air intrusions and their relation to strong surface winds in extratropical cyclones...and intro to synoptic and meso-scale cyclone dynamics Shira Raveh-Rubin and Heini Wernli Institute

The benefits and developments in ensemble wind forecasting

The benefits and developments in ensemble wind forecasting Erik Andersson Slide 1 ECMWF European Centre for Medium-Range Weather Forecasts Slide 1 ECMWF s global forecasting system High resolution forecast

VARIED FLOW IN OPEN CHANNELS

Chapter 15 Open Channels vs. Closed Conduits VARIED FLOW IN OPEN CHANNELS Fluid Mechanics, Spring Term 2011 In a closed conduit there can be a pressure gradient that drives the flow. An open channel has

CONVECTION-ALLOWING SIMULATIONS OF COLD POOLS IN THE NORTHWESTERN SAHARA

COSMO User Seminar, Langen, 4th March 2008 CONVECTION-ALLOWING SIMULATIONS OF COLD POOLS IN THE NORTHWESTERN SAHARA 1 Peter Knippertz, 1 Jörg Trentmann & 2 Axel Seifert 1 Institute for Atmospheric Physics,

Vertical structure. To conclude, we will review the critical factors invloved in the development of extratropical storms.

Vertical structure Now we will examine the vertical structure of the intense baroclinic wave using three visualization tools: Upper level charts at selected pressure levels Vertical soundings for selected

Part-8c Circulation (Cont)

Part-8c Circulation (Cont) Global Circulation Means of Transfering Heat Easterlies /Westerlies Polar Front Planetary Waves Gravity Waves Mars Circulation Giant Planet Atmospheres Zones and Belts Global

Examination #3 Wednesday, 28 November 2001

Name & Signature Dr. Droegemeier Student ID Meteorology 1004 Introduction to Meteorology Fall, 2001 Examination #3 Wednesday, 28 November 2001 BEFORE YOU BEGIN!! Please be sure to read each question CAREFULLY

MET 4300/5355 Severe Weather

MET 4300/5355 Severe Weather Lecture 1 Introduction Course Organization Tu/Th 11:00AM-12:15 PM, AHC5 Rm357 Haiyan Jiang, 305-348-2984, AHC5 Rm371, haiyan.jiang@fiu.edu Office Hours Tu 12:15-1:15 PM, or

A new operational convection-permitting NWP system for tropical cyclone forecasting in the SW Indian Ocean

A new operational convection-permitting NWP system for tropical cyclone forecasting in the SW Indian Ocean Olivier BOUSQUET, Soline BIELLI, David BARBARY, Marie-Dominique LEROUX, Christelle BARTHE, Dominique

Ki-Hong Min 1*, Seonhee Choo 2, and Gyuwon Lee 1, and Kyung-Eak Kim 1,3

Ki-Hong Min 1*, Seonhee Choo 2, and Gyuwon Lee 1, and Kyung-Eak Kim 1,3 1 School of Earth System Sciences, Major in Atmospheric Science, Kyungpook National University, Daegu, South Korea 2 Forecast Technology

Seamless Probabilistic Forecasts for Civil Protection: from week to minutes

Seamless Probabilistic Forecasts for Civil Protection: from week to minutes Yong Wang, Clemens Wastl, Andre Simon, Mihaly Szűcs ZAMG and HMS An EU project Bridging of Probabilistic Forecasts and Civil

Thunderstorms and Severe Weather. (Chapt 15)

Thunderstorms and Severe Weather (Chapt 15) The Big Picture We ve emphasized horizontal transport of energy to balance the planetary energy budget: Hadley Cell Subtropical divergence Midlatitude cyclones

Multi-scale Predictability Aspects of a Severe European Winter Storm

1 Multi-scale Predictability Aspects of a Severe European Winter Storm NASA MODIS James D. Doyle, C. Amerault, P. A. Reinecke, C. Reynolds Naval Research Laboratory, Monterey, CA Mesoscale Predictability

Application and verification of ECMWF products 2011

Application and verification of ECMWF products 2011 National Meteorological Administration 1. Summary of major highlights Medium range weather forecasts are primarily based on the results of ECMWF and

Weather report 28 November 2017 Campinas/SP

Weather report 28 November 2017 Campinas/SP Summary: 1) Synoptic analysis and pre-convective environment 2) Verification 1) Synoptic analysis and pre-convective environment: At 1200 UTC 28 November 2017

A SEVERE WEATHER EVENT IN ROMANIA DUE TO MEDITERRANEAN CYCLONIC ACTIVITY

A SEVERE WEATHER EVENT IN ROMANIA DUE TO MEDITERRANEAN CYCLONIC ACTIVITY Florinela Georgescu, Gabriela Bancila, Viorica Dima National Meteorological Administration, Bucharest, Romania Abstract Mediterranean

Helen Titley and Rob Neal

Processing ECMWF ENS and MOGREPS-G ensemble forecasts to highlight the probability of severe extra-tropical cyclones: Storm Doris UEF 2017, 12-16 June 2017, ECMWF, Reading, U.K. Helen Titley and Rob Neal

Weather and Climate Basics

Weather and Climate Basics Laura Boekel Forecaster at Bureau of Meteorology Aims of this presentation To describe what I do as a forecaster at the Bureau of Meteorology To provide an interesting introduction

What drives snowstorms and seasonal snowfall amounts in Colorado?

What drives snowstorms and seasonal snowfall amounts in Colorado? Russ S. Schumacher Colorado State Climatologist Director, Colorado Climate Center Department of Atmospheric Science, Colorado State University

Modelling Black Saturday

Modelling Black Saturday M 1 ( ) e R ε er School of Mathematical Sciences Monash University and Chermelle Engel (School of Earth Sciences, University of Melbourne) Todd Lane (School of Earth Sciences,

P10.5 Water flows down a rectangular channel that is 4 ft wide and 3 ft deep. The flow rate is 15,000 gal/min. Estimate the Froude number of the flow.

P10.5 Water flows down a rectangular channel that is 4 ft wide and ft deep. The flow rate is 15,000 gal/min. Estimate the Froude number of the flow. Solution: Convert the flow rate from 15,000 gal/min

P4.9 THE SEVERE THUNDERSTORM OUTBREAK IN FINLAND ON 5 JULY 2002

P4.9 THE SEVERE THUNDERSTORM OUTBREAK IN FINLAND ON 5 JULY 2002 Ari-Juhani Punkka* and Jenni Teittinen Finnish Meteorological Institute, Helsinki, Finland 1. INTRODUCTION On 5 July 2002 a fast propagating

Dynamical Processes Related to Cyclone Evolution near Greenland

Dynamical Processes Related to Cyclone Evolution near Greenland Ragnhild B. Skeie a, Jón Egill Kristjánsson a, Haraldur Ólafsson b a Department of Geosciences, University of Oslo b University of Iceland

Weather and Climate Basics

Aims of this presentation Weather and Climate Basics To describe what I do as a forecaster at the Bureau of Meteorology Laura Boekel Forecaster at Bureau of Meteorology To provide an interesting introduction

DOWNSLOPE WINDSTORM IN ICELAND WRF/MM5 MODEL COMPARISON-I

DOWNSLOPE WINDSTORM IN ICELAND WRF/MM5 MODEL COMPARISON-I Ólafur Rögnvaldsson 1,2, Jian Wen Bao 3, Hálfdán Ágústsson 1,4 and Haraldur Ólafsson 1,2,4 1 Institute for Meteorological Research, Reykjavík,

http://www.ssec.wisc.edu/data/composites.html Red curve: Incoming solar radiation Blue curve: Outgoing infrared radiation. Three-cell model of general circulation Mid-latitudes: 30 to 60 latitude MID-LATITUDES

National Institute of Water and Atmospheric Research (NIWA)

National Institute of Water and Atmospheric Research (NIWA) Michael Uddstrom 1, Mike Revell, Stuart Moore, Ed Yang, Richard Turner, Sam Dean, Tony Bromley, Ben Liley, & Simon Vosper 2 1 Principal Scientist:

High Resolution Numerical Weather Prediction for High Impact and Extreme Weather Events in 2014 across Southern California

High Resolution Numerical Weather Prediction for High Impact and Extreme Weather Events in 2014 across Southern California Alex Tardy Alexander.Tardy@noaa.gov NWS San Diego Warning Coordination Meteorologist

NUMERICAL SIMULATION OF FLOW OVER TWO DIMENSIONAL MOUNTAIN RIDGE USING SIMPLE ISENTROPIC MODEL

NUMERICAL SIMULATION OF FLOW OVER TWO-DIMENSIONAL MOUNTAIN RIDGE 1, 2 1 Graduate School of Climate Sciences, University of Bern 2 National Agency for Meteorology, Climatology and Geophysics, Republic of

Summary of November Central U.S. Winter Storm By Christopher Hedge

Summary of November 12-13 2010 Central U.S. Winter Storm By Christopher Hedge Event Overview The first significant snowfall of the 2010-2011 season affected portions of the plains and upper Mississippi

Final Report for Partners Project S Project Title: Application of High Resolution Mesoscale Models to Improve Weather Forecasting in Hawaii

Final Report for Partners Project S04-44687 Project Title: Application of High Resolution Mesoscale Models to Improve Weather Forecasting in Hawaii University: University of Hawaii Name of University Researcher

2 July 2013 Flash Flood Event

2 July 2013 Flash Flood Event By Richard H. Grumm and Charles Ross National Weather Service State College, PA 1. Overview A retrograding 500 hpa cyclone and anticyclone (Fig. 1) set up deep southerly flow

AVIATION APPLICATIONS OF A NEW GENERATION OF MESOSCALE NUMERICAL WEATHER PREDICTION SYSTEM OF THE HONG KONG OBSERVATORY

P452 AVIATION APPLICATIONS OF A NEW GENERATION OF MESOSCALE NUMERICAL WEATHER PREDICTION SYSTEM OF THE HONG KONG OBSERVATORY Wai-Kin WONG *1, P.W. Chan 1 and Ivan C.K. Ng 2 1 Hong Kong Observatory, Hong

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

Synoptic Meteorology II: Frontogenesis Examples Figure 1

Synoptic Meteorology II: Frontogenesis Examples The below images, taken from the 1200 UTC 17 January 2019 GFS forecast run, provide examples of the contributions of deformation and divergence to frontogenesis.

Master thesis in meteorology, oceanography and climate, 30 hp. Case study of CAT over the North Atlantic Ocean. Kristoffer Molarin

Master thesis in meteorology, oceanography and climate, 30 hp Case study of CAT over the North Atlantic Ocean Kristoffer Molarin Supervisors: Tomas Mårtensson and Gunilla Svensson Department of Meteorology

THUNDERSTORMS. Convective heavy rain accompanied by lightning and thunder. Ahrens

THUNDERSTORMS Convective heavy rain accompanied by lightning and thunder Ahrens Thunderstorms About 1,800 T-storms occur around the world at any instant Where do they occur the most? National Lightning

Polar Lows and other High Latitude Weather Systems. John Turner and Tom Bracegirdle British Antarctic Survey Cambridge, UK

Polar Lows and other High Latitude Weather Systems John Turner and Tom Bracegirdle British Antarctic Survey Cambridge, UK A mosaic of infra-red satellite imagery of the Antarctic and Southern Ocean on

Winter Storm of 15 December 2005 By Richard H. Grumm National Weather Service Office State College, PA 16803

Winter Storm of 15 December 2005 By Richard H. Grumm National Weather Service Office State College, PA 16803 1. INTRODUCTION A complex winter storm brought snow, sleet, and freezing rain to central Pennsylvania.

TWO CASES OF HEAVY RAIN ON THE MEDITERRANEAN SIDE OF THE ALPS IN MAP. Robert Houze 1 and Socorro Medina University of Washington

1.1 TWO CASES OF HEAVY RAIN ON THE MEDITERRANEAN SIDE OF THE ALPS IN MAP Robert Houze 1 and Socorro Medina University of Washington Matthias Steiner Princeton University 1. INTRODUCTION The Mesoscale Alpine

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

Shawn M. Milrad Atmospheric Science Program Department of Geography University of Kansas Lawrence, Kansas

Shawn M. Milrad Atmospheric Science Program Department of Geography University of Kansas Lawrence, Kansas Eyad H. Atallah and John R. Gyakum Department of Atmospheric and Oceanic Sciences McGill University

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs ESCI 322: 3 s.h. Environmental Hydrology ESCI 241: 4 s.h. Meteorology (G2, L)

ESCI 110: 2 s.h. Introduction to Earth Sciences Programs General introduction to each of the earth sciences disciplines and to college life. 2 hrs. lec. Offered in fall. Restricted to earth sciences majors.

LACE - PROBLEMS IN DYNAMICS & COUPLING AND SOME SOLUTIONS

Regional Cooperation for Limited Area Modeling in Central Europe LACE - PROBLEMS IN DYNAMICS & COUPLING AND SOME SOLUTIONS Petra Smolíková (CHMI) with contribution from many colleagues Summary Dynamics:

Mid Atlantic Heavy rainfall event 1. Overview 2. Methods and Data 3. Pattern

1. Overview Mid Atlantic Heavy rainfall event With an inertial gravity wave? By Richard H. Grumm National Weather Service, State College, PA 16803 Contributions from the Albany MAP An unseasonably strong

Goals of this Chapter

Waves in the Atmosphere and Oceans Restoring Force Conservation of potential temperature in the presence of positive static stability internal gravity waves Conservation of potential vorticity in the presence

APPLICATIONS OF SEA-LEVEL PRESSURE

APPLICATIONS OF SEA-LEVEL PRESSURE RETRIEVAL FROM SCATTEROMETER WINDS Jérôme Patoux, Ralph C. Foster and Robert A. Brown OVWST meeting Seattle, November 20, 2008 Pressure retrieval: how does it work? model

A polar low named Vera

4/2009 Meteorology A polar low named Vera dynamics and model performance Thor Erik Nordeng 3 Background 20th November 2008 the Norwegian Meteorological Institute issued an extreme weather warning for

MESO-NH cloud forecast verification with satellite observation

MESO-NH cloud forecast verification with satellite observation Jean-Pierre CHABOUREAU Laboratoire d Aérologie, University of Toulouse and CNRS, France http://mesonh.aero.obs-mip.fr/chaboureau/ DTC Verification

Identification of Convective Hotspots in Mountainous Terrain

Identification of Convective Hotspots in Mountainous Terrain Martin Hagen, Leslie Grebe, Joël van Baelen, Evelyne Richard DLR Oberpfaffenhofen, Germany Université de Clermont-Ferrand, France Observatoire

Estimation of satellite observations bias correction for limited area model

Estimation of satellite observations bias correction for limited area model Roger Randriamampianina Hungarian Meteorological Service Budapest, Hungary roger@met.hu ITSC-XV, Maratea,, Italy, 4-104 October

Identification of Predictors for Nowcasting Heavy Rainfall In Taiwan --------------------- Part II: Storm Characteristics and Nowcasting Applications Challenges in Developing Nowcasting Applications for

Features of the wind fields associated with Typhoon 0418 (Songda) compared with those of Typhoon 9119 (Mireille)

Features of the wind fields associated with Typhoon 0418 (Songda) compared with those of Typhoon 9119 (Mireille) by Fumiaki Fujibe 1, Naoko Kitabatake 2, Kotaro Bessho 2 and Shunsuke Hoshino 3 ABSTRACT

Isolated severe weather and cold air damming 9 November 2005 By Richard H. Grumm National Weather Service Office State College, PA 16801

Isolated severe weather and cold air damming 9 November 2005 By Richard H. Grumm National Weather Service Office State College, PA 16801 1. INTRODUCTION Two lines of convection moved over the State of

An overview of Wet Season Forecasting in the Northern Territory

TWP-ICE Meeting November 2004 An overview of Wet Season Forecasting in the Northern Territory Lori Chappel Northern Territory Regional Forecasting Centre Australian Government Bureau of Meteorology Day

Forecasting Polar Lows. Gunnar Noer The Norwegian Meteorological Institute in Tromsø

Forecasting Polar Lows Gunnar Noer The Norwegian Meteorological Institute in Tromsø Longyearbyen Hopen Bear Island Jan Mayen Tromsø Gunnar Noer Senior forecaster / developer for polar meteorology The Norwegian

Lightning Data Assimilation using an Ensemble Kalman Filter

Lightning Data Assimilation using an Ensemble Kalman Filter G.J. Hakim, P. Regulski, Clifford Mass and R. Torn University of Washington, Department of Atmospheric Sciences Seattle, United States 1. INTRODUCTION

Current Status of COMS AMV in NMSC/KMA

Current Status of COMS AMV in NMSC/KMA Eunha Sohn, Sung-Rae Chung, Jong-Seo Park Satellite Analysis Division, NMSC/KMA soneh0431@korea.kr COMS AMV of KMA/NMSC has been produced hourly since April 1, 2011.

1. COLD FRONT - CLOUD STRUCTURE IN SATELLITE IMAGES

1. COLD FRONT - CLOUD STRUCTURE IN SATELLITE IMAGES The satellite image shows a cyclonically curved synoptic scale cloud band usually a few hundred kilometres wide; in the VIS image the cloud band mostly

Tropical Storms & Hurricanes Part 1. August 1992

Lecture #16 (April 5, 2010, Monday) Tropical Storms & Hurricanes Part 1 August 1992 Tracks of rain accumulation & clouds from Hurricane Rita September 2005 Tropical Cyclones Around the Globe Why none here?

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

Tropical Meteorology. Roger K. Smith INDO IR

Tropical Meteorology Roger K. Smith INDO IR 01010510 1 GMS IR 01022621 GOES IR 00112909 2 Introduction to the tropics The zonal mean circulation (Hadley circulation) The data network in the tropics (field

Lee Vortices. Craig C. Epifanio. Introduction. Stratified Flow Past Topography: Basic Phenomenology

Epifanio, C. C.: Lee Vortices in Encyclopedia of the Atmospheric Sciences, Cambridge University Press, 1150-1160. Lee Vortices Craig C. Epifanio National Center for Atmospheric Research, Boulder, Colorado

Chapter 1 Anatomy of a Cyclone

Chapter 1 Anatomy of a Cyclone The Beast in the East 15-17 February 2003 Extra-tropical cyclone an area of low pressure outside of the tropics Other names for extra-tropical cyclones: Cyclone Mid-latitude

Mid Atlantic Severe Event of 1 May 2017 Central Pennsylvania QLCS event By Richard H. Grumm National Weather Service, State College, PA 16803

1. Overview Mid Atlantic Severe Event of 1 May 2017 Central Pennsylvania QLCS event By Richard H. Grumm National Weather Service, State College, PA 16803 A strong upper-level wave (Fig.1) moving into a