Ulrike Romatschke, Robert Houze, Socorro Medina

Slides:



Advertisements
Similar presentations
500 km. Adapted from Fink and Reiner (2003) Squall Line Generation 12.5°-20°N 5°-12.5°N Mid-level Vortex What do we know about the AEW-MCS Relationship?
Advertisements

Robert Houze University of Washington (with contributions from B. Smull) Winter MONEX Summer MONEX Presented at: International Conference on MONEX and.
A Spatial Climatology of Convection in the Northeast U.S. John Murray and Brian A. Colle National Weather Service, WFO New York NY Stony Brook University,
R. A. Houze, Jr., U. Romatschke K. L. Rasmussen AGU Fall Meeting, Remote Sensing of Natural Hazards, San Francisco, 9 Dec 2011 Mesoscale Aspects of Storms.
Precipitation Over Continental Africa and the East Atlantic: Connections with Synoptic Disturbances Matthew A. Janiga November 8, 2011.
The Convective Cloud Population during the Buildup of the Madden- Julian Oscillation AGU Fall Meeting, San Francisco, 7 December 2011 R. Houze, S. Brodzik,
Structure of mid-latitude cyclones crossing the California Sierra Nevada as seen by vertically pointing radar Socorro Medina, Robert Houze, Christopher.
February 5th, TRMM Conference The 3-D Reflectivity Structure of Intense Atlantic Hurricanes as seen by the TRMM PR Deanna Hence, Robert Houze.
Deanna Hence, Stacy Brodzik and Robert Houze University of Washington Introduction Methodology TCSP Storms RAINEX Storms Combined TCSP + RAINEX Storms.
Synoptic, Topographic, and Diurnal Effects on Summer Convection in South America Ulrike Romatschke University of Washington, University of Vienna Robert.
Scientific Objectives and Required Facilities Socorro Medina, Robert Houze, and Stacy Brodzik TIMREX Planning Meeting, Tainan, Taiwan, 9 November 2007.
Robert A. Houze, Jr., Darren C. Wilton, and Bradley F. Smull University of Washington Robert A. Houze, Jr., Darren C. Wilton, and Bradley F. Smull University.
Pakistan Flood 2010: P. J. Webster R. A. Houze, Jr. P. J. Webster R. A. Houze, Jr. International Weather & Climate Events of 2010, AMS Annual Meeting,
Radar-Observed Characteristics of the Diurnal Cycle of Precipitation during NAME 2004 Timothy Lang, Steve Nesbitt, Rob Cifelli, and Steve Rutledge Colorado.
Mesoscale Convective Systems: Recent Observational and Diagnostic Studies Robert Houze Department of Atmospheric Sciences University of Washington 10 th.
The Effect of the Terrain on Monsoon Convection in the Himalayan Region Socorro Medina 1, Robert Houze 1, Anil Kumar 2,3 and Dev Niyogi 3 Conference on.
The Effect of the Terrain on Monsoon Convection in the Himalayan Region Socorro Medina 1, Robert Houze 1, Anil Kumar 2,3 and Dev Niyogi 3 Cloud and Precipitation.
U.S.-Taiwan Meeting, Boulder, 30 October 2006 Study of Intense Convection over Taiwan: Some Food for Thought R. Houze Study of Intense Convection over.
Extreme Convection Near the Himalayas and Andes Gerald R. North Symposium, Texas A&M University, College Station, June 8, 2009 Robert A. Houze, Jr. Ulrike.
Extreme Convection in South America as Seen by TRMM Ulrike Romatschke 1, 2 and Robert A. Houze, Jr. 1 1 University of Washington, 2 University of Vienna.
Hydrometeors Injected into the Large-scale Environment by Tropical Cloud Systems Robert A. Houze & Courtney Schumacher Co-PIs ARM Science Team Meeting,
Understanding Atmospheric Heating in the GPM Era Robert Houze University of Washington 6 th GPM International Planning Workshop, 6-8 November 2006, Annapolis,
The effect of terrain and land surface on summer monsoon convection in the Himalayan region Socorro Medina, Robert Houze, Anil Kumar, and Dev Niyogi 13.
The Tropical Cloud Population R. A. Houze Lecture, Indian Institute of Tropical Meteorology, Pune, 9 August 2010.
Schumacher and Houze (2006) This Lecture: Review of Schumacher and Houze, 2006: Stratiform precipitation over sub- Saharan Africa and the Tropical.
Cirrus Production by Tropical Mesoscale Convective Systems Jasmine Cetrone and Robert Houze 8 February 2008.
Mesoscale Convective Systems Robert Houze Department of Atmospheric Sciences University of Washington Nebraska Kansas Oklahoma Arkansas.
Cirrus Production by Tropical Mesoscale Convective Systems Jasmine Cetrone and Robert Houze University of Washington Motivation Atmospheric heating by.
TiMREX Meeting, Boulder, 13 September 2007WesternCentral Eastern UW TiMREX Orographic Precipitation Study Houze, Medina, Brodzik UW TiMREX Orographic Precipitation.
Extreme Convection Near the Himalayas and Andes PMM Science Team Meeting, Salt Lake City, October 28, 2009 Robert A. Houze, Jr. Ulrike Romatschke, Socorro.
TRMM Observations of Convection over the Himalayan Region R. A. Houze and D. C. Wilton University of Washington Presented 1 February 2005 at the International.
The tropical convective cloud population Peking University Seminar, Beijing, 4 July 2011 Robert Houze University of Washington.
Diurnal Variability of Deep Tropical Convection R. A. Houze Lecture, Summer School on Severe and Convective Weather, Nanjing, July 2011.
Diurnal Variability of Deep Tropical Convection R. A. Houze Lecture, Indian Institute of Tropical Meteorology, Pune, 12 August 2010.
Mesoscale Convective Systems: Recent Observational and Diagnostic Studies Robert Houze Department of Atmospheric Sciences University of Washington.
Robert A. Houze University of Washington Robert A. Houze University of Washington Using the TRMM Precipitation Radar for Storm Structure Analysis Precipitation.
Mesoscale Convective System Heating and Momentum Feedbacks R. Houze NCAR 10 July 2006.
Global Variability of Mesoscale Convective System Anvil Structure Jian Yuan Jasmine Cetrone Robert A. Houze, Jr. ARM Cloud Modeling Working Group, Princeton,
Orographic triggering and mesoscale organization of extreme storms in subtropical South America Kristen Lani Rasmussen Robert A. Houze, Jr. ICAM 2013,
Satellite Radar Studies of Extreme Convective Storms ? ? New Fellows Presentation, AGU, San Francisco, 5 December 2012 Robert A. Houze, Jr. University.
MJO is: A convective disturbance that initiates over the tropical Indian Ocean and propagates eastward. MJO “wave” can propagate around the entire tropics.
The mesoscale organization and dynamics of extreme convection in subtropical South America Kristen Lani Rasmussen Robert A. Houze, Jr., Anil Kumar 2013.
Validation of TRMM rainfall products at Gadanki T. Narayana Rao NARL, Gadanki K. Nakamura, HyARC, Nagoya, Japan D. Narayana Rao, NARL, Gadanki National.
CAPE AND LIGHTNING How is distribution of CAPE more diffused than distribution of lightning? Positive corelation between convective cloud layer, columnar.
25N 30N 65E75E65E75E65E75E Height (km) 8 Distance (km)
Yuying Zhang, Jim Boyle, and Steve Klein Program for Climate Model Diagnosis and Intercomparison Lawrence Livermore National Laboratory Jay Mace University.
The MJO Cloud Population over the Indian Ocean
Joanna Futyan and Tony DelGenio GIST 25, Exeter, 24 th October 2006 The Evolution of Convective Systems over Africa and the Tropical Atlantic.
MJO Insights from the S-PolKa radar in DYNAMO Robert A. Houze, Jr. H. C. Barnes, S. W. Powell, A. K. Rowe, M. Zuluaga University of Washington Symposium.
Orographic Precipitation in Potentially Unstable Alpine Storms: MAP IOPs 2b, 3, and 5 Socorro Medina and Robert A. Houze.
Diurnal Cycle of Cloud and Precipitation Associated with the North American Monsoon System Pingping Xie, Yelena Yarosh, Mingyue Chen, Robert Joyce, John.
A complicated mesoscale convective system Lightning flashes (ICs, CGs) happen both inside and outside convective regions (“cells”), sometimes in stratiform.
1 Spatio-temporal Distribution of Latent Heating in the Southeast Asian Monsoon Region School of Earth and Atmospheric Sciences Georgia Institute of Technology.
Floods in Pakistan and India 2010 Robert A. Houze, Jr. with S. Medina, U. Romatschke, K. Rasmussen, S. Brodzik, D. Niyogi, and A. Kumar Robert A. Houze,
Global Distribution of Different Forms of Convection as Seen by TRMM Robert A. Houze, Jr. University of Washington with: K. L. Rasmussen, M. D. Zuluaga,
University Allied Workshop (1-3 July, 2008)
Tropical and subtropical convection in South Asia and South America
Maritime Continent Convection
Hannah C. Barnes, Robert A. Houze, Jr., and Manuel D. Zuluaga
Radar/Surface Quantitative Precipitation Estimation
The Variable Structure of Convection at Low Latitudes
M. D. Zuluaga and R. A. Houze, Jr. University of Washington
Ulrike Romatschke University of Washington, University of Vienna
MJO Modulation of Lightning in Mesoscale Convective Systems
Katrina Virts and Robert A. Houze, Jr. University of Washington
Jennifer C. DeHart, Robert A. Houze, Jr. and Deanna A. Hence
Phil Arkin, ESSIC University of Maryland
Pre-Monsoon Monsoon TRMM PR data reveal the nature of the convection producing extreme monsoon rains In the monsoon: Deep cores shift from Bengal to Pakistan.
Mesoscale Convective Systems Observed by CloudSat
Ming-Dah Chou Department of Atmospheric Sciences
Presentation transcript:

Ulrike Romatschke, Robert Houze, Socorro Medina Regional, Seasonal and Diurnal Variations of Convection in the Asian Monsoon Region Authors Ulrike Romatschke, Robert Houze, Socorro Medina Clouds and Precipitation Seminar, University of Washington, 15 November 2007

Region of Study

Outline Dataset Comparison with Houze et al. Premonsoon – Monsoon Introduction Dataset Regonal Variations Comparison with Houze et al. Seasonal Variations Premonsoon – Monsoon Diurnal Variations Dependence on topography Conclusion and future Work

Dataset TRMM Precipitation Radar (PR), Version 6 Products 2A23: Radar Rain Characteristics 2A25: Radar Rainfall Rate and Profile Monsoon Season: June - September 1999-2001 2004-2006 Premonsoon Season: May 1999-2006

Data Processing Gridspacing Interpolation on Cartesian Grid horizontal: ~5 km vertical: 250 m Search for individual systems contiguous pixels define system characteristic parameters (e.g. time, location, size,…)

Definitions Deep Intense Convective Cores 20 16 12 8 4 Definitions Height [km] Deep Intense Convective Cores 40 dBZ echo > 10 km in hight Wide Intense Convective Cores 40 dBZ echo area > 1,000 km² Broad Stratiform Echos area > 50,000 km² 0 42.5 85 Distance [km] 24 22 20 Latitude 84 86 88 90 Longitude 15 20 Latitude 90 95 [dBZ] Longitude

Objectives Compare with Houze et al. (2007) Extend dataset geographical region Premonsoon Season Diurnal Cycle Find especially active regions

Outline Dataset Comparison with Houze et al. Premonsoon – Monsoon Introduction Dataset Regonal Variations Comparison with Houze et al. Seasonal Variations Premonsoon – Monsoon Diurnal Variations Dependence on topography Conclusion and future Work

Comparison Deep Intense Convective Cores 1999-2001/2004-2006 2002-2003

Large Scale Flow Patterns during Monsoon 1000 mb 700 mb 40 30 20 10 60 70 80 90 100/60 70 80 90 100 Terrain [km]

Comparison Wide Intense Convective Cores 1999-2001/2004-2006 2002-2003

Comparison Broad Stratiform Systems 1999-2001/2004-2006 2002-2003

Outline Dataset Comparison with Houze et al. Premonsoon – Monsoon Introduction Dataset Regonal Variations Comparison with Houze et al. Seasonal Variations Premonsoon – Monsoon Diurnal Variations Dependence on topography Conclusion and future Work

Deep Intense Convective Cores Premonsoon Monsoon

The Indian Dry-Line Weston (1971) 1000 mb 700 mb Surface p [mb] and v 500 mb v Weston (1971)

The Indian Dry-Line 200 mb 700 mb 1000 mb Monsoon Premonsoon

Wide Intense Convective Cores Premonsoon Monsoon

Wide vs. Deep Intense Convective Cores Premonsoon Premonsoon

Wide vs. Deep Intense Convective Cores Monsoon Monsoon

Wide vs. Deep Intense Convective Cores Ganges Delta Monsoon

Broad Stratiform Systems Premonsoon Monsoon

Broad Stratiform Systems Rain Climatology Monsoon Xie et al. (2006)

Outline Dataset Comparison with Houze et al. Premonsoon – Monsoon Introduction Dataset Regonal Variations Comparison with Houze et al. Seasonal Variations Premonsoon – Monsoon Diurnal Variations Dependence on topography Conclusion and future Work

Diurnal Cycle, Monsoon

Diurnal Cycle

Diurnal Cycle

Diurnal Cycle, Monsoon

Diurnal Cycle Deep Intense Convective Cores Monsoon

Diurnal Cycle Deep Intense Convective Cores Monsoon

Diurnal Cycle Deep Intense Convective Cores Monsoon

Diurnal Cycle Deep Intense Convective Cores Monsoon

Diurnal Cycle Deep Intense Convective Cores Premonsoon

Diurnal Cycle Deep Intense Convective Cores Premonsoon Surface p [mb] and v Weston (1971) Xie et al. (2006)

Diurnal Cycle, Deep Intense Convective Cores, Premonsoon Zuidema (2002) Mean percent high cloudiness Cloud Top < 210 K May – September 1999

Diurnal Cycle, Monsoon

Diurnal Cycle, Monsoon Wide Intense Convective Cores 1999-2001 vs 1999-2001 2004-2006

Diurnal Cycle Wide Intense Convective Cores Monsoon

Diurnal Cycle Wide Intense Convective Cores Monsoon Xie et al. (2006)

Diurnal Cycle Wide Intense Convective Cores Premonsoon - Monsoon

Diurnal Cycle Wide Intense Convective Cores Premonsoon

Diurnal Cycle, Monsoon

Diurnal Cycle, Monsoon

Diurnal Cycle Broad Stratiform Systems Monsoon

Diurnal Cycle Broad Stratiform Systems Monsoon

Diurnal Cycle Broad Stratiform Systems Monsoon

Diurnal Cycle Broad Stratiform Systems Monsoon Williams and Houze (1987)

Outline Dataset Comparison with Houze et al. Premonsoon – Monsoon Introduction Dataset Regonal Variations Comparison with Houze et al. Seasonal Variations Premonsoon – Monsoon Diurnal Variations Dependence on topography Conclusion and future Work

Conclusions Larger independent dataset seems to confirm Houze et al. (2007) Premonsoon – Monsoon • Shift in places of occurrence of Deep and Wide Intense Convective Cores. • More Wide Intense Convective Cores and Broad Stratiform Systems over the ocean during Monsoon. Diurnal Cycles • Strong afternoon peak in Deep Intense Convective Cores. • Afternoon and night peaks in Wide Intense Convective Cores. • Evening minimum in Broad Stratiform Systems. Rain climatology compares • with Broad Stratiform Systems over the ocean. • with Wide Intense Convective Cores at the Himalayan Foothills. • not with Deep Intense Convective Cores.

Conclusions Larger independent dataset seems to confirm Houze et al. (2007) Premonsoon – Monsoon • Shift in places of occurrence of Deep and Wide Intense Convective Cores. • More Wide Intense Convective Cores and Broad Stratiform Systems over the ocean during Monsoon. Diurnal Cycles • Strong afternoon peak in Deep Intense Convective Cores. • Afternoon and night peaks in Wide Intense Convective Cores. • Evening minimum in Broad Stratiform Systems. Rain climatology compares • with Broad Stratiform Systems over the ocean. • with Wide Intense Convective Cores at the Himalayan Foothills. • not with Deep Intense Convective Cores. This is just the beginning!

Future Work Get 2002/2003 Version 6 data. Statistics for other variables. Look at specific regions • physical background • different variable fields (e.g. wind) • satellite data

Variables Orbitnumber Number of convective pixels Date Time Number of pixels 3D Number of pixels 2D Latitude Longitude Height Longest horizontal dimension Height of terrain Area Number of convective pixels Number of stratiform pixels Convective, stratiform, total • rain rate • volumetric rain rate • rain fraction • area fraction

Future Work Get 2002/2003 Version 6 data. Statistics for other variables. Look at specific regions • physical background • different variable fields (e.g. wind) • satellite data

Future Work