Robert Houze University of Washington (with contributions from B. Smull)
|
|
|
- Marybeth Newton
- 5 years ago
- Views:
Transcription
1 Robert Houze University of Washington (with contributions from B. Smull) Winter MONEX Summer MONEX Presented at: International Conference on MONEX and its Legacy, 3-7 Feb 2005, New Delhi
2 Johnson & Houze 1987
3 WINTER MONEX Diurnal variation of high cloudiness near Borneo Bintulu S. CHINA SEA December 1978 BORNEO 08 LST 20 LST 14 LST 02 LST Houze et al. 1981
4 Radar Obs.. of WINTER MONEX Borneo cloud system Bintulu Stratiform Precipitation Houze et al. 1981
5 Diurnal gravity wave generation of mesoscale convection over coastal South America Pacific Andes South America Pacific Andes South America Mapes et al. 2003
6 Johnson & Houze 1987
7 Percent High Cloudiness in the Summer Monsoon May-September 1999 < 235 K < 210 K 850 mb wind 300 mb wind & sfc pressure Zuidema 2002
8 Diurnal cycle, mean percent high cloudiness, 1999 Cloud Top < 210 K Zuidema 2002
9 Location of cloud systems by horizontal dimension May-September 1999 Cloud Top < 210 K r < 85 km r = km r = km r > 210 km Zuidema 2002
10 Webster et al NOAA Ship Ronald H. Brown
11 JASMINE Mesoscale Convective Systems Defined & tracked by 218 K infrared threshold Zuidema 2002
12 JASMINE 1999, Ship Track & Satellite Data E Ship Track Webster et al. 2002
13
14 IR Temperature 08:30 LST
15 IR Temperature 11:30 LST
16 IR Temperature 14:30 LST
17 IR Temperature 17:30 LST
18 IR Temperature 20:30 LST
19 IR Temperature 20:30 LST Ship radar
20 JASMINE 1999 Ship Radar Data 2345 LST 22 May LST 23 May LST 23 May 99
21 JASMINE 1999 Ship Radar Data Reflectivity Reflectivity Doppler Radial Velocity 22 May LST
22 JASMINE 1999 Ship Radar Data Reflectivity Reflectivity Doppler Radial Velocity 22 May LST
23 23 May LST JASMINE Ship Radar Data TRMM Precipitation Radar Swath
24 TRMM Precipitation Radar shows extensive stratiform structure 23 May LST
25 SUMMER MONEX 6 July mb wind Houze & Churchill 1987
26 SUMMER MONEX 6 July 1979 NOAA P3 Aircraft 20N Microphysics 20N Radar 14N 14N 88E 92E 88E 92E Houze & Churchill 1987
27 SUMMER MONEX 8 July mb wind Houze & Churchill 1987
28 SUMMER MONEX 8 July 1979 NOAA P3 Aircraft 20N Microphysics Radar 20N 16N 16N 82E 86E 82E 86E Houze & Churchill 1987
29 SUMMER MONEX Microphysics, All P3 flights, 3-8 July 1979 Flight Level Temperature (deg C) Columns Columns Needles Plates Plates & Dendrites Dendrites Melting Aggregates & Drops Aggregates Drops Relative Frequency of Occurrence Houze & Churchill 1987
30 TRMM Precipitation Radar June-Sept, Intense Convective Wide Stratiform N E
31 Oceanic convection in both winter and summer monsoons occur in deep, broad mesoscale convective systems, often diurnally forced Ground and airborne radars showed that precipitation in the mature mesoscale convective systems was predominantly stratiform Microphysical data collected by aircraft confirmed the highly stratiform character of the precipitation, with evidence of ice particle growth by vapor deposition & aggregation JASMINE 1999 shows the deepest, broadest, & longest lasting mesoscale systems are diurnal & propagate southward, possibly as waves, with discrete jumps in the progression of the cloud systems TRMM satellite radar data (since 1997) confirm the stratiform character of the precipitation over the ocean in contrast to that over the land
32
33
34
35
36 Diurnal cycle, mean percent high cloudiness, 1999 <235 K <210 K Zuidema 2002
37
38 Stratiform precipitation shown by the Bintulu Radar Churchill & Houze 1984
39 WINTER MONEX Time series of high cloudiness seen by satellite SOUTH CHINA SEA BORNEO December 1978 Houze et al. 1981
Introduction to tropical meteorology and deep convection
Introduction to tropical meteorology and deep convection TMD Lecture 1 Roger K. Smith University of Munich A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical
On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic
On Surface fluxes and Clouds/Precipitation in the Tropical Eastern Atlantic Chris Fairall, NOAA/ESRL Paquita Zuidema, RSMAS/U Miami with contributions from Peter Minnett & Erica Key AMMA Team Meeting Leeds,
Introduction to tropical meteorology and deep convection
Introduction to tropical meteorology and deep convection Roger K. Smith University of Munich A satpix tour of the tropics The zonal mean circulation (Hadley circulation), Inter- Tropical Convergence Zone
Aircraft Observations for ONR DRI and DYNAMO. Coupled Air-sea processes: Q. Wang, D. Khelif, L. Mahrt, S. Chen
Aircraft Observations for ONR DRI and DYNAMO (NOAA/ONR/NSF) Coupled Air-sea processes: Q. Wang, D. Khelif, L. Mahrt, S. Chen Deep convection/mjo initiation: Dave Jorgensen, S. Chen, R. Houze Aerosol/Cloud
The Properties of Convective Clouds Over the Western Pacific and Their Relationship to the Environment of Tropical Cyclones
The Properties of Convective Clouds Over the Western Pacific and Their Relationship to the Environment of Tropical Cyclones Principal Investigator: Dr. Zhaoxia Pu Department of Meteorology, University
Characteristics of extreme convection over equatorial America and Africa
Characteristics of extreme convection over equatorial America and Africa Manuel D. Zuluaga, K. Rasmussen and R. A. Houze Jr. Atmospheric & Climate Dynamics Seminar Department of Atmospheric Sciences, University
Myung-Sook Park, Russell L. Elsberry and Michael M. Bell. Department of Meteorology, Naval Postgraduate School, Monterey, California, USA
Latent heating rate profiles at different tropical cyclone stages during 2008 Tropical Cyclone Structure experiment: Comparison of ELDORA and TRMM PR retrievals Myung-Sook Park, Russell L. Elsberry and
EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphe
EPIC2001 was conceived as an intensive process study along and near 95 o W during September and October 2001 used to make measurements of the atmosphere and ocean in this region. Two aircraft, the National
Vertical Motion in Near-Equatorial Winter Monsoon Convection
682 Journal of the Meteorological Society of Japan Vol. 60, No. 2 Vertical Motion in Near-Equatorial Winter Monsoon Convection By Richard H. Johnson Department of Atmospheric Science, Colorado State University
Interannual Variations of Arctic Cloud Types:
Interannual Variations of Arctic Cloud Types: Relationships with Sea Ice and Surface Temperature Ryan Eastman Stephen Warren University of Washington Department of Atmospheric Sciences Changes in Arctic
Chapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs. Bright band associated with stratiform precipitation in a squall line system
Chapter 3 Convective Dynamics Part V ñ Bright Bands, Bow Echoes and MCCs Photographs Todd Lindley (This part contains materials taken from UCAR MCS training module) Bright band associated with stratiform
BMKG Research on Air sea interaction modeling for YMC
BMKG Research on Air sea interaction modeling for YMC Prof. Edvin Aldrian Director for Research and Development - BMKG First Scientific and Planning Workshop on Year of Maritime Continent, Singapore 27-3
October 1986 R. H. Johnson 721. Lower-Tropospheric Warming and Drying in Tropical Mesoscale Convective Systems:
October 1986 R. H. Johnson 721 Lower-Tropospheric Warming and Drying in Tropical Mesoscale Convective Systems: Implications for the Problem of Cumulus Parameterization By Richard H. Johnson Department
Climate Dynamics (PCC 587): Feedbacks & Clouds
Climate Dynamics (PCC 587): Feedbacks & Clouds DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 6: 10-14-13 Feedbacks Climate forcings change global temperatures directly
Identification of Predictors for Nowcasting Heavy Rainfall In Taiwan --------------------- Part II: Storm Characteristics and Nowcasting Applications Challenges in Developing Nowcasting Applications for
30th Conference on Hurricanes and Tropical Meteorology, April 2012, Ponte Vedra Beach, Florida
Characteristics of Extreme Summer Convection in the Tropical Americas Manuel ld D. Zuluaga and Robert ta A. Houze Jr. University of Washington 30th Conference on Hurricanes and Tropical Meteorology, 15
J1.2 OBSERVED REGIONAL AND TEMPORAL VARIABILITY OF RAINFALL OVER THE TROPICAL PACIFIC AND ATLANTIC OCEANS
J1. OBSERVED REGIONAL AND TEMPORAL VARIABILITY OF RAINFALL OVER THE TROPICAL PACIFIC AND ATLANTIC OCEANS Yolande L. Serra * JISAO/University of Washington, Seattle, Washington Michael J. McPhaden NOAA/PMEL,
Life Cycle of Convective Systems over Western Colombia
Life Cycle of Convective Systems over Western Colombia Meiry Sakamoto Uiversidade de São Paulo, São Paulo, Brazil Colombia Life Cycle of Convective Systems over Western Colombia Convective System (CS)
CLOUD AND PRECIPITATION PROCESSES OBSERVED IN THE DECEMBER 2001 STORM STUDIED OVER THE OREGON CASCADES IN IMPROVE
7.2 CLOUD AND PRECIPITATION PROCESSES OBSERVED IN THE 13-14 DECEMBER 2001 STORM STUDIED OVER THE OREGON CASCADES IN IMPROVE Christopher P. Woods, Mark T. Stoelinga, John D. Locatelli, Peter V. Hobbs *
Diurnal Characteristics of Precipitation Features over the Tropical East Pacific: A Comparison of the EPIC and TEPPS Regions
4068 J O U R N A L O F C L I M A T E VOLUME 21 Diurnal Characteristics of Precipitation Features over the Tropical East Pacific: A Comparison of the EPIC and TEPPS Regions R. CIFELLI Colorado State University,
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (December 2017)
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (December 2017) 1. Review of Regional Weather Conditions for November 2017 1.1 In November 2017, Southeast Asia experienced inter-monsoon conditions in the first
MCS cloud life cycle from merged satellite data
MCS cloud life cycle from merged satellite data Dominique Bouniol1, Thomas Fiolleau2, Rémy Roca2,Patrick Raberanto3 1 CNRM, CNRS/Météo-France, Toulouse, France 2 LEGOS, CNRS/IRD/CNES/Université Paul Sabatier,
Chapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes
Chapter 3 Convective Dynamics 3.4. Bright Bands, Bow Echoes and Mesoscale Convective Complexes Photographs Todd Lindley Bright band associated with stratiform precipitation in a squall line system 1 Bright
The TRMM Precipitation Radar s View of Shallow, Isolated Rain
OCTOBER 2003 NOTES AND CORRESPONDENCE 1519 The TRMM Precipitation Radar s View of Shallow, Isolated Rain COURTNEY SCHUMACHER AND ROBERT A. HOUZE JR. Department of Atmospheric Sciences, University of Washington,
Mentor: Edward Zipser Professor, Atmospheric Sciences University of Utah. Presenter: Petra Miku
Presenter: Petra Miku Mentor: Edward Zipser Professor, Atmospheric Sciences University of Utah Split Workshop in Atmospheric Physics and Oceanography, May 22-28, 2011 Split, Croatia 1. Part I: convective
Oceanic Eddies in the VOCALS Region of the Southeast Pacific Ocean
Oceanic Eddies in the VOCALS Region of the Southeast Pacific Ocean Outline: Overview of VOCALS Dudley B. Chelton Oregon State University Overview of the oceanographic component of VOCALS Preliminary analysis
Climate Dynamics (PCC 587): Clouds and Feedbacks
Climate Dynamics (PCC 587): Clouds and Feedbacks D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C E S D A Y 7 : 1
The Diurnal Cycle of Convection over the Northern South China Sea
December Journal of the 2008 Meteorological Society of Japan, S.L. Vol. AVES 86, and No. R.H. 6, pp. JOHNSON 919 934, 2008 919 The Diurnal Cycle of Convection over the Northern South China Sea Steven L.
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
Global sea surface temperature October 25 th 2007
The VOCALS Regional Experiment Aerosols, clouds, and precipitation in southeast Pacific stratocumulus Robert Wood Atmospheric Sciences University of Washington Global sea surface temperature October 25
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (September 2017)
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (September 2017) 1. Review of Regional Weather Conditions in August 2017 1.1 Southwest Monsoon conditions continued to prevail in the region in August 2017. The
Observational analysis of storms and flooding events in the Pacific Northwest. Introduction
Observational analysis of storms and flooding events in the Pacific Northwest Jake Crouch UNCA ATMS Class of 2007 April 18, 2009 Cloud and Precipitation Processes and Patterns Group Introduction Average
The Climatology of Clouds using surface observations. S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences.
The Climatology of Clouds using surface observations S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences Gill-Ran Jeong Cloud Climatology The time-averaged geographical distribution of cloud
A "New" Mechanism for the Diurnal Variation of Convection over the Tropical Western Pacific Ocean
A "New" Mechanism for the Diurnal Variation of Convection over the Tropical Western Pacific Ocean D. B. Parsons Atmospheric Technology Division National Center for Atmospheric Research (NCAR) Boulder,
Atmospheric Boundary Layer over Land, Ocean, and Ice. Xubin Zeng, Michael Brunke, Josh Welty, Patrick Broxton University of Arizona
Atmospheric Boundary Layer over Land, Ocean, and Ice Xubin Zeng, Michael Brunke, Josh Welty, Patrick Broxton University of Arizona xubin@email.arizona.edu 24 October 2017 Future of ABL Observations Workshop
CHAPTER 2 DATA AND METHODS. Errors using inadequate data are much less than those using no data at all. Charles Babbage, circa 1850
CHAPTER 2 DATA AND METHODS Errors using inadequate data are much less than those using no data at all. Charles Babbage, circa 185 2.1 Datasets 2.1.1 OLR The primary data used in this study are the outgoing
L. McMurdie, R. Houze, J. Zagrodnik, W. Petersen, M. Schwaller
L. McMurdie, R. Houze, J. Zagrodnik, W. Petersen, M. Schwaller International Atmospheric Rivers Conference, San Diego, CA, 9 August 2016 Goals of OLYMPEX Validate GPM satellite radar and passive microwave
February 1992 R. H. Johnson 353. Heat and Moisture Sources and Sinks of Asian Monsoon. By Richard H. Johnson
February 1992 R. H. Johnson 353 Heat and Moisture Sources and Sinks of Asian Monsoon Precipitating Systems By Richard H. Johnson Department of Atmospheric Science, Colorado State University, Fort Collins
Comparison of the seasonal cycle of tropical and subtropical precipitation over East Asian monsoon area
21st International Congress on Modelling and Simulation, Gold Coast, Australia, 29 Nov to 4 Dec 2015 www.mssanz.org.au/modsim2015 Comparison of the seasonal cycle of tropical and subtropical precipitation
Robert Rogers, Sylvie Lorsolo, Paul Reasor, John Gamache, and Frank Marks Monthly Weather Review January 2012
Introduction Data & Methodology Results Robert Rogers, Sylvie Lorsolo, Paul Reasor, John Gamache, and Frank Marks Monthly Weather Review January 2012 SARAH DITCHEK ATM 741 02.01.16 Introduction Data &
Characterizing the Structure of Hurricane Karl (2010): Doppler Radar and WRF
Characterizing the Structure of Hurricane Karl (2010): Doppler Radar and WRF Jennifer DeHart and Robert Houze Atmospheric Physics and Chemistry Seminar 5.9.16 NASA grants: NNX13AG71G / NNX12AJ82G Orographic
Comparison of Diurnal Variation of Precipitation System Observed by TRMM PR, TMI and VIRS
Comparison of Diurnal Variation of Precipitation System Observed by TRMM PR, TMI and VIRS Munehisa K. Yamamoto, Fumie A. Furuzawa 2,3 and Kenji Nakamura 3 : Graduate School of Environmental Studies, Nagoya
Cloud parameterization and cloud prediction scheme in Eta numerical weather model
Cloud parameterization and cloud prediction scheme in Eta numerical weather model Belgrade, 10th September, 2018 Ivan Ristić, CEO at Weather2 Ivana Kordić, meteorologist at Weather2 Introduction Models
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
Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation
Interpretation of Polar-orbiting Satellite Observations Outline Polar-Orbiting Observations: Review of Polar-Orbiting Satellite Systems Overview of Currently Active Satellites / Sensors Overview of Sensor
How to display RGB imagery by SATAID
How to display RGB imagery by SATAID Akihiro SHIMIZU Meteorological Satellite Center (MSC), Japan Meteorological Agency (JMA) Ver. 2015110500 RGB imagery on SATAID SATAID software has a function of overlapping
Aircraft Observations of Tropical Cyclones. Robert Rogers NOAA/AOML Hurricane Research Division Miami, FL
Aircraft Observations of Tropical Cyclones Robert Rogers NOAA/AOML Hurricane Research Division Miami, FL 1 Motivation Why are observations important? Many important physical processes within hurricanes
Rogers and Yau Chapter 12: Precipitation Processes (emphasizing stratiform rain convection and severe storms will be next lecture)
Rogers and Yau Chapter 12: Precipitation Processes (emphasizing stratiform rain convection and severe storms will be next lecture) There is a relationship between the scale of atmospheric vertical motions
Vertical motion in the stratiform precipitation region observed with Equatorial Atmospheric Radar (EAR)
Vertical motion in the stratiform precipitation region observed with Equatorial Atmospheric Radar (EAR) NISHI Noriyuki (Kyoto Univ.) with: M.K. Yamamoto, T. Shimomai, S. Mori, A. Hamada, S. Fukao SOWER
A more detailed and quantitative consideration of organized convection: Part I Cold pool dynamics and the formation of squall lines
A more detailed and quantitative consideration of organized convection: Part I Cold pool dynamics and the formation of squall lines Note: Lecture notes presented here based on course Daily Weather Laboratory
Electrification of Stratiform Regions in Mesoscale Convective Systems. Part I: An Observational Comparison of Symmetric and Asymmetric MCSs
VOL. 57, NO. 13 JOURNAL OF THE ATMOSPHERIC SCIENCES 1JULY 2000 Electrification of Stratiform Regions in Mesoscale Convective Systems. Part I: An Observational Comparison of Symmetric and Asymmetric MCSs
ture and evolution of the squall line developed over the China Continent. We made data analysis of the three Doppler radar observation during the IFO
Simulation Experiment of Squall Line Observed in the Huaihe River Basin, China Kazuhisa Tusboki 1 and Atsushi Sakakibara 2 1 Hydrospheric Atmospheric Research Center, Nagoya University 2 Research Organization
The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter
The HIAPER Cloud Radar Performance and Observations During Winter Storm Observations of a Nor easter S. Ellis 1*, R. Rauber 2, P. Tsai 1, J. Emmett 1, E. Loew 1, C. Burghart 1, M. Dixon 1, J. Vivekanandan
A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S
A synthesis of published VOCALS studies on marine boundary layer and cloud structure along 20S Chris Bretherton Department of Atmospheric Sciences University of Washington VOCALS RF05, 72W 20S Work summarized
REVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre)
WORLD METEOROLOGICAL ORGANIZATION Distr.: RESTRICTED CBS/OPAG-IOS (ODRRGOS-5)/Doc.5, Add.5 (11.VI.2002) COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS ITEM: 4 EXPERT
Assimilate W88D Doppler Vr for Humberto 05
Assimilate W88D Doppler Vr for Humberto 05 WRF/EnKF Forecast vs. Observations vs. 3DVAR Min SLP Max wind The WRF/3DVAR (as a surrogate of operational algorithm) assimilates the same radar data but without
2006/12/29. MISMO workshop Yokohama, 25 November, 2008
Global cloud-resolving simulations of MJO events in November 2006 - January 2007 ---multiscale structure --- 2006/12/29 MTSAT-1R NICAM Tomoe NASUNO, Masaki SATOH, Hiroaki MIURA, NICAM development group
Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Large-Eddy Simulations of Tropical Convective Systems, the Boundary Layer, and Upper Ocean Coupling Eric D. Skyllingstad
Diurnal Characteristics of Precipitation Features Over the East Pacific: A. Comparison of the EPIC and TEPPS Regions. Colorado State University
Diurnal Characteristics of Precipitation Features Over the East Pacific: A Comparison of the EPIC and TEPPS Regions R. Cifelli* 1, S.W. Nesbitt 2, S.A. Rutledge 1, W.A. Petersen 3, and S. Yuter 4 1 Colorado
HY-2A Satellite User s Guide
National Satellite Ocean Application Service 2013-5-16 Document Change Record Revision Date Changed Pages/Paragraphs Edit Description i Contents 1 Introduction to HY-2 Satellite... 1 2 HY-2 satellite data
Day Microphysics RGB Nephanalysis in daytime. Meteorological Satellite Center, JMA
Day Microphysics RGB Nephanalysis in daytime Meteorological Satellite Center, JMA What s Day Microphysics RGB? R : B04 (N1 0.86) Range : 0~100 [%] Gamma : 1.0 G : B07(I4 3.9) (Solar component) Range :
WMO Aeronautical Meteorology Scientific Conference 2017
Session 1 Science underpinning meteorological observations, forecasts, advisories and warnings 1.1 En route phenomena 1.1.1 Ice crystal icing, and airframe icing research Signatures of supercooled liquid
P1.6 Simulation of the impact of new aircraft and satellite-based ocean surface wind measurements on H*Wind analyses
P1.6 Simulation of the impact of new aircraft and satellite-based ocean surface wind measurements on H*Wind analyses Timothy L. Miller 1, R. Atlas 2, P. G. Black 3, J. L. Case 4, S. S. Chen 5, R. E. Hood
P1.3 DIURNAL VARIABILITY OF THE CLOUD FIELD OVER THE VOCALS DOMAIN FROM GOES IMAGERY. CIMMS/University of Oklahoma, Norman, OK 73069
P1.3 DIURNAL VARIABILITY OF THE CLOUD FIELD OVER THE VOCALS DOMAIN FROM GOES IMAGERY José M. Gálvez 1, Raquel K. Orozco 1, and Michael W. Douglas 2 1 CIMMS/University of Oklahoma, Norman, OK 73069 2 NSSL/NOAA,
11D.6 DIURNAL CYCLE OF TROPICAL DEEP CONVECTION AND ANVIL CLOUDS: GLOBAL DISTRIBUTION USING 6 YEARS OF TRMM RADAR AND IR DATA
11D.6 DIURNAL CYCLE OF TROPICAL DEEP CONVECTION AND ANVIL CLOUDS: GLOBAL DISTRIBUTION USING 6 YEARS OF TRMM RADAR AND IR DATA 1. INTRODUCTION Before the launch of the TRMM satellite in late 1997, most
Key Laboratory of Mesoscale Severe Weather, Ministry of Education, School of Atmospheric Sciences, Nanjing University
Modeling Rapid Intensification of Typhoon Saomai (2006) with the Weather Research and Forecasting Model and Sensitivity to Cloud Microphysical Parameterizations Jie Ming and Yuan Wang Key Laboratory of
Weather Studies Introduction to Atmospheric Science
Weather Studies Introduction to Atmospheric Science American Meteorological Society Chapter 1 Monitoring The Weather Credit: This presentation was prepared for AMS by Michael Leach, Professor of Geography
On Trade-Wind Cumulus Cold Pools
On Trade-Wind Cumulus Cold Pools Paquita Zuidema & Zhujun Li U of Miami Reg Hill, Ludovic Bariteau, Bob Rilling, Chris Fairall, Alan Brewer, Bruce Albrecht, Jeff Hare AGU Dec 2011 key finding from RICO:
NOTES AND CORRESPONDENCE. A Pronounced Continental-Scale Diurnal Mode of the Asian Summer Monsoon
462 MONTHLY WEATHER REVIEW VOLUME 128 NOTES AND CORRESPONDENCE A Pronounced Continental-Scale Diurnal Mode of the Asian Summer Monsoon T. N. KRISHNAMURTI AND C. M. KISHTAWAL Department of Meteorology,
What makes the Arctic hot?
1/3 total USA UN Environ Prog What makes the Arctic hot? Local communities subsistence Arctic Shipping Routes? Decreasing Ice cover Sept 2007 -ice extent (Pink=1979-2000 mean min) Source: NSIDC Oil/Gas
Eight Years of TRMM Data: Understanding Regional Mechanisms Behind the Diurnal Cycle
Eight Years of TRMM Data: Understanding Regional Mechanisms Behind the Diurnal Cycle Steve Nesbitt, Rob Cifelli, Steve Rutledge Colorado State University Chuntao Liu, Ed Zipser University of Utah Funding
Comparison of Convection Characteristics at the Tropical Western Pacific Darwin Site Between Observation and Global Climate Models Simulations
Comparison of Convection Characteristics at the Tropical Western Pacific Darwin Site Between Observation and Global Climate Models Simulations G.J. Zhang Center for Atmospheric Sciences Scripps Institution
Convective Systems of the North Australian Monsoon
1OCTOBER 2008 P O P E E T A L. 5091 Convective Systems of the North Australian Monsoon MICK POPE Bureau of Meteorology Training Centre, Bureau of Meteorology, Melbourne, Victoria, Australia CHRISTIAN JAKOB
Climate FDDA. Andrea Hahmann NCAR/RAL/NSAP February 26, 2008
Climate FDDA Andrea Hahmann NCAR/RAL/NSAP hahmann@ucar.edu February 26, 2008 Outline Climate downscaling - the basics Method (ATEC ranges) - Climo-FDDA Possible application of Climo-FDDA data at the ranges
Diurnal cycles of precipitation, clouds, and lightning in the tropics from 9 years of TRMM observations
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L04819, doi:10.1029/2007gl032437, 2008 Diurnal cycles of precipitation, clouds, and lightning in the tropics from 9 years of TRMM observations Chuntao Liu 1 and Edward
Measurements of Raindrop Size Distributions over the Pacific Warm Pool and Implications for Z R Relations
847 Measurements of Raindrop Size Distributions over the Pacific Warm Pool and Implications for Z R Relations SANDRA E. YUTER AND ROBERT A. HOUZE JR. (Manuscript received 23 January 1996, in final form
The Rainfall System Classification over the Korean Peninsula Using TRMM TMI and Ground Measurement Data
6 th International Precipitation Working Group Workshop-São José dos Campos- October 15~19, 2012 The Rainfall System Classification over the Korean Peninsula Using TRMM TMI and Ground Measurement Data
Modulation of the diurnal cycle of tropical deep convective clouds
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L20704, doi:10.1029/2006gl027752, 2006 Modulation of the diurnal cycle of tropical deep convective clouds by the MJO Baijun Tian, 1 Duane
MJO and Diurnal Cycle Experiment (MODEX): The proposed YMC-NCAR aircraft and ground deployment
MJO and Diurnal Cycle Experiment (MODEX): The proposed YMC-NCAR aircraft and ground deployment Courtney Schumacher (Texas A&M), Shuyi Chen and Chidong Zhang (U. Miami) MJO in the MC Weakens over islands
Remote Sensing of Precipitation
Lecture Notes Prepared by Prof. J. Francis Spring 2003 Remote Sensing of Precipitation Primary reference: Chapter 9 of KVH I. Motivation -- why do we need to measure precipitation with remote sensing instruments?
ROLE OF CLOUD RADIATION INTERACTION IN THE DIURNAL VARIATION OF PRECIPITATION
ROLE OF CLOUD RADIATION INTERACTION IN THE DIURNAL VARIATION OF PRECIPITATION SETHU RAMAN AND ADRIENNE WOOTTEN DEPARTMENT OF MARINE, EARTH AND ATMOSPHERIC SCIENCES NORTH CAROLINA STATE UNIVERSITY, RALEIGH,
Northwest Outlook October 2016
Northwest Outlook October 2016 Rainfall Opportunities and Challenges Rainfall over the month of September presented some challenges for the fall harvest while other producers benefitted. Figure 1a shows
GPS Meteorology at Japan Meteorological Agency
GPS Meteorology at Japan Meteorological Agency Masahito Ishihara Japan Meteorological Agency CIMO Expert Team on Remote Sensing Upper-Air Technology and Techniques 14-17 March, 2005 Geneva, Switzerland
WRF Model Simulated Proxy Datasets Used for GOES-R Research Activities
WRF Model Simulated Proxy Datasets Used for GOES-R Research Activities Jason Otkin Cooperative Institute for Meteorological Satellite Studies Space Science and Engineering Center University of Wisconsin
We suspect the answer is a little bit of both these explanations. There is likely substantial under-reporting of severe weather in regions with either
RELAMPAGO (Remote sensing of Electrification, Lightning, And Meso-scale/micro-scale Processes with Adaptive Ground Observations) - Relevance to NASA GPM GV Relampago means lightning in both Spanish and
Understanding the Microphysical Properties of Developing Cloud Clusters during TCS-08
DISTRIBUTION STATEMENT A: Approved for public release; distribution is unlimited. Understanding the Microphysical Properties of Developing Cloud Clusters during TCS-08 PI: Elizabeth A. Ritchie Department
Journal of Climate. Convective Variability associated with the Boreal Summer Intraseasonal Oscillation in the South China Sea Region
Journal of Climate Convective Variability associated with the Boreal Summer Intraseasonal Oscillation in the South China Sea Region --Manuscript Draft-- Manuscript Number: Full Title: Article Type: Corresponding
1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely
CHAPTER 3 SOLAR AND TERRESTRIAL RADIATION MULTIPLE CHOICE QUESTIONS 1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely 2. is the distance between successive
Improved rainfall and cloud-radiation interaction with Betts-Miller-Janjic cumulus scheme in the tropics
Improved rainfall and cloud-radiation interaction with Betts-Miller-Janjic cumulus scheme in the tropics Tieh-Yong KOH 1 and Ricardo M. FONSECA 2 1 Singapore University of Social Sciences, Singapore 2
2.2 Sounding composite construction. 2.3 Vertical velocity retrieval
7.1 DROPSONDE DERIVED STRUCTURE OF MESOSCALE CONVECTIVE SYSTEMS OBSERVED DURING BAMEX James Correia Jr and R. W. Arritt ; Dept. of Agronomy, Iowa State University, Ames, IA 1. Introduction The Bow echo
Mechanical Turbulence Wind forms eddies as it blows around hanger, stands of trees or other obstructions
Turbulence Low-level Turbulence below 15,000 feet consists of Mechanical Turbulence Convective Turbulence Frontal Turbulence Wake Turbulence Mechanical Turbulence Wind forms eddies as it blows around hanger,
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO
Ship-Based Measurements of Cloud Microphysics and PBL Properties in Precipitating Trade Cumuli During RICO Institutions: University of Miami; University of Colorado; NOAA ETL Investigators: P. Kollias
TROPICAL-EXTRATROPICAL INTERACTIONS
Notes of the tutorial lectures for the Natural Sciences part by Alice Grimm Fourth lecture TROPICAL-EXTRATROPICAL INTERACTIONS Anomalous tropical SST Anomalous convection Anomalous latent heat source Anomalous
Object-based approaches for exploring high-resolution simulations
GEWEX Convection-Permitting Climate Modeling Meeting, Boulder, Colorado, 6-8 Sept 2016 Object-based approaches for exploring high-resolution simulations Jean-Pierre CHABOUREAU Laboratoire d Aérologie,
Supplementary Figure 1. Summer mesoscale convective systems rainfall climatology and trends. Mesoscale convective system (MCS) (a) mean total
Supplementary Figure 1. Summer mesoscale convective systems rainfall climatology and trends. Mesoscale convective system (MCS) (a) mean total rainfall and (b) total rainfall trend from 1979-2014. Total
APPLICATION OF WEATHER MODIFICTION TECHNOLOGY FOR FLOOD PREVENTION IN JAKARTA 2013
APPLICATION OF WEATHER MODIFICTION TECHNOLOGY FOR FLOOD PREVENTION IN JAKARTA 2013 Tri Handoko SETO and Heru WIDODO Weather Modification Technology Center, Agency for the Asessment and Application of Technology
Intercomparison of Satellite Precipitation Products for Different Cloud Types
8 th IPWG & 5 th IWSSM Joint Workshop Bologna, 3-7 October, 2016 Intercomparison of Satellite Precipitation Products for Different Cloud Types Nobuyuki UTSUMI Hyungjun Kim, Taikan OKI (IIS, The University
Precipitation Structure and Processes of Typhoon Nari (2001): A Modeling Propsective
Precipitation Structure and Processes of Typhoon Nari (2001): A Modeling Propsective Ming-Jen Yang Institute of Hydrological Sciences, National Central University 1. Introduction Typhoon Nari (2001) struck
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018)
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018) 1. Review of Regional Weather Conditions for January 2018 1.1 The prevailing Northeast monsoon conditions over Southeast Asia strengthened in January
Recent Data Assimilation Activities at Environment Canada
Recent Data Assimilation Activities at Environment Canada Major upgrade to global and regional deterministic prediction systems (now in parallel run) Sea ice data assimilation Mark Buehner Data Assimilation