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ageostrophic flow and jet streak dynamics PowerPoint PPT Presentation
ageostrophic flow and jet streak dynamics - Koch, http://legacy.ncsu.edu/classes/mea444-sekoch ... Circulations during Heavy Snow Events along the East Coast of the United States. ...
Koch, http://legacy.ncsu.edu/classes/mea444-sekoch ... Circulations during Heavy Snow Events along the East Coast of the United States. ...
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Barrier jets and other lowlevel jets a description of types and causes PowerPoint PPT Presentation
Barrier jets and other lowlevel jets a description of types and causes - Schwerdtfeger (1975, 1979) describes a barrier jet along the ... as an ageostrophic response to the damming of stably-stratified flow by the Sierra Nevada. ...
Schwerdtfeger (1975, 1979) describes a barrier jet along the ... as an ageostrophic response to the damming of stably-stratified flow by the Sierra Nevada. ...
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Imbalance and Vertical Motion PowerPoint PPT Presentation
Imbalance and Vertical Motion - In order for wind to flow in a cyclonically curved manner, (an acceleration) it ... An isallobar is a line of equal change in atmospheric pressure. ...
In order for wind to flow in a cyclonically curved manner, (an acceleration) it ... An isallobar is a line of equal change in atmospheric pressure. ...
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SO441 Synoptic Meteorology PowerPoint PPT Presentation
SO441 Synoptic Meteorology - SO441 Synoptic Meteorology. Fronts. Lesson 8: Weeks 13-14. ... The Great Plains dry line is a sharp change in air masses but is not considered a ... lifting air cools ...
SO441 Synoptic Meteorology. Fronts. Lesson 8: Weeks 13-14. ... The Great Plains dry line is a sharp change in air masses but is not considered a ... lifting air cools ...
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Propagation of a Front, Encountering a Cold Air Layer PowerPoint PPT Presentation
Propagation of a Front, Encountering a Cold Air Layer - Frontogenesis. Sawyer-Eliassen Equation. Model. Result. Discussion ... Frontogenesis. Geostrophic. confluence of temperature field due to geostrophic wind field ...
Frontogenesis. Sawyer-Eliassen Equation. Model. Result. Discussion ... Frontogenesis. Geostrophic. confluence of temperature field due to geostrophic wind field ...
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Severe Thunderstorm Summary METR 361 PowerPoint PPT Presentation
Severe Thunderstorm Summary METR 361 - Severe Thunderstorm Summary METR 361 The Pre-storm Environment On the Surface map, look for: Warm air, T 50 F High dew points 50 F Triggers a.
Severe Thunderstorm Summary METR 361 The Pre-storm Environment On the Surface map, look for: Warm air, T 50 F High dew points 50 F Triggers a.
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Geostrophic and thermal wind PowerPoint PPT Presentation
Geostrophic and thermal wind - Geostrophic and thermal wind Reminder Geostrophic wind in pressure coordinates In the free atmosphere, wind is usually close to geostrophic. The departure from ...
Geostrophic and thermal wind Reminder Geostrophic wind in pressure coordinates In the free atmosphere, wind is usually close to geostrophic. The departure from ...
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Q-G Theory: Using the Q-Vector PowerPoint PPT Presentation
Q-G Theory: Using the Q-Vector - Q-G Theory: Using the Q-Vector Patrick Market Department of Atmospheric Science University of Missouri-Columbia Advanced Synoptic M. D. Eastin Summary: Review of ...
Q-G Theory: Using the Q-Vector Patrick Market Department of Atmospheric Science University of Missouri-Columbia Advanced Synoptic M. D. Eastin Summary: Review of ...
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Vorticity and Jets PowerPoint PPT Presentation
Vorticity and Jets - Positive vorticity advection (PVA) ... Anticyclonic Vorticity Advection ... Positive (cyclonic) vorticity advection leads to upper level divergence, and rising motion ...
Positive vorticity advection (PVA) ... Anticyclonic Vorticity Advection ... Positive (cyclonic) vorticity advection leads to upper level divergence, and rising motion ...
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The Quasi-Geostrophic Omega Equation (without friction and diabatic terms) PowerPoint PPT Presentation
The Quasi-Geostrophic Omega Equation (without friction and diabatic terms) - THE TRENBERTH (1978) INTERPRETATION The Quasi-Geostrophic Omega Equation (without friction and diabatic terms) PROBLEM: TERM 1 and 2 on the RHS are often large and ...
THE TRENBERTH (1978) INTERPRETATION The Quasi-Geostrophic Omega Equation (without friction and diabatic terms) PROBLEM: TERM 1 and 2 on the RHS are often large and ...
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Parameterization of surface stress direction PowerPoint PPT Presentation
Parameterization of surface stress direction - Solved pressure bias by increasing vertical diffusion - Destroyes vertical ... on stability and roughness, turn surface stress in geostrophic direction ...
Solved pressure bias by increasing vertical diffusion - Destroyes vertical ... on stability and roughness, turn surface stress in geostrophic direction ...
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Jet%20Stream%20Circulations PowerPoint PPT Presentation
Jet%20Stream%20Circulations - Jet Stream Circulations. April 16, 2004. Tools. Vorticity advection. Thermal advection ... is relatively easy to measure.VORTICITY. Vorticity & Vertical Motion ...
Jet Stream Circulations. April 16, 2004. Tools. Vorticity advection. Thermal advection ... is relatively easy to measure.VORTICITY. Vorticity & Vertical Motion ...
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Rotating Fluid -Part II A PowerPoint PPT Presentation
Rotating Fluid -Part II A - Rotating Fluid -Part II A GFD view of the Ocean and the Atmosphere (a follow up Raymond s Lectures) Arnaud Czaja
Rotating Fluid -Part II A GFD view of the Ocean and the Atmosphere (a follow up Raymond s Lectures) Arnaud Czaja
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Frontogenesis Forcing and Banded Precipitation PowerPoint PPT Presentation
Frontogenesis Forcing and Banded Precipitation - Title: Mesoscale Organization of Wintertime Precipitation Author: pbanacos Last modified by: PBANACOS Created Date: 9/20/2001 12:02:09 AM Document presentation format
Title: Mesoscale Organization of Wintertime Precipitation Author: pbanacos Last modified by: PBANACOS Created Date: 9/20/2001 12:02:09 AM Document presentation format
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Jet Stream PowerPoint PPT Presentation
Jet Stream - ... temperature where the cold polar air moving towards the equator ... Consider, the case of no wind near the surface (the 1000 mb surface is ... Cold air ...
... temperature where the cold polar air moving towards the equator ... Consider, the case of no wind near the surface (the 1000 mb surface is ... Cold air ...
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Sin ttulo de diapositiva PowerPoint PPT Presentation
Sin ttulo de diapositiva - Sin ttulo de diapositiva
Sin ttulo de diapositiva
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Upper-Level Frontogenesis PowerPoint PPT Presentation
Upper-Level Frontogenesis - Upper-Level Frontogenesis Cliff Mass University of Washington * Remotely Sensed Ozone During an Upper Level Front Simulated PV Structure at Same Time Good correlation ...
Upper-Level Frontogenesis Cliff Mass University of Washington * Remotely Sensed Ozone During an Upper Level Front Simulated PV Structure at Same Time Good correlation ...
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The Christmas Day Snowstorm of 2002 PowerPoint PPT Presentation
The Christmas Day Snowstorm of 2002 - The Christmas Day Snowstorm of 2002
The Christmas Day Snowstorm of 2002
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Evaluating Skill in Ocean Model Parameterizations: Taylor Diagrams PowerPoint PPT Presentation
Evaluating Skill in Ocean Model Parameterizations: Taylor Diagrams - http://isotherm.rsmas.miami.edu/~nick. HFIP Observations ... Track and Intensity of TC's Gustav and Ike Versus AXBTs relative to OHC and 26oC Isotherm Depth. ...
http://isotherm.rsmas.miami.edu/~nick. HFIP Observations ... Track and Intensity of TC's Gustav and Ike Versus AXBTs relative to OHC and 26oC Isotherm Depth. ...
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The Need for and Feasibility of a Global Lightning Detection Network PowerPoint PPT Presentation
The Need for and Feasibility of a Global Lightning Detection Network - The Need for and Feasibility of a Global Lightning Detection Network Frederick R. Mosher NWS/NCEP Aviation Weather Center
The Need for and Feasibility of a Global Lightning Detection Network Frederick R. Mosher NWS/NCEP Aviation Weather Center
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Split Fronts and Cold Fronts Aloft PowerPoint PPT Presentation
Split Fronts and Cold Fronts Aloft - The causes for 'prefrontal squall lines' have been mysteries to meteorologists ... Crawford (1950): no prefrontal instability lines of any importance over the ...
The causes for 'prefrontal squall lines' have been mysteries to meteorologists ... Crawford (1950): no prefrontal instability lines of any importance over the ...
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CSTAR NetMeeting Presentation Split Fronts in the Cold Air Damming Region PowerPoint PPT Presentation
CSTAR NetMeeting Presentation Split Fronts in the Cold Air Damming Region - CSTAR NetMeeting Presentation Split Fronts in the Cold Air Damming Region
CSTAR NetMeeting Presentation Split Fronts in the Cold Air Damming Region
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A Comparison of Vertical Motions Obtained from Different Forms of the Omega Equation Christopher J' PowerPoint PPT Presentation
A Comparison of Vertical Motions Obtained from Different Forms of the Omega Equation Christopher J' - Current Affiliation: Department of Soils, Environmental, and Atmospheric Sciences ... cyclone development accompanied by upper-air wave merger over North America (Nov. ...
Current Affiliation: Department of Soils, Environmental, and Atmospheric Sciences ... cyclone development accompanied by upper-air wave merger over North America (Nov. ...
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The northward retreat of the MeiYu front and the formation of the lowlevel jet PowerPoint PPT Presentation
The northward retreat of the MeiYu front and the formation of the lowlevel jet - strong potential vorticity anomaly with mature MYF, Mei-Yu frontogenesis by CISK. ... Mei-yu frontogenesis. 7 (b) 850 hPa ... Frontogenesis and cyclogenesis ...
strong potential vorticity anomaly with mature MYF, Mei-Yu frontogenesis by CISK. ... Mei-yu frontogenesis. 7 (b) 850 hPa ... Frontogenesis and cyclogenesis ...
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Objectives PowerPoint PPT Presentation
Objectives - Instability: not required for light snow (2-4 inches) but definitely needed for ... Part II: Frontal Forcing of an Extreme Snow Event, MWR, 329-348. ...
Instability: not required for light snow (2-4 inches) but definitely needed for ... Part II: Frontal Forcing of an Extreme Snow Event, MWR, 329-348. ...
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Synoptic-scale forcing mechanisms PowerPoint PPT Presentation
Synoptic-scale forcing mechanisms - My talk to MSC and NCEP - Feb 2006 ... Ervin Zsoter ECMWF, Meteorological Operations Section ervin.zsoter@ecmwf.int
My talk to MSC and NCEP - Feb 2006 ... Ervin Zsoter ECMWF, Meteorological Operations Section ervin.zsoter@ecmwf.int
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Variability of the Atlantic North Equatorial Countercurrent NECC PowerPoint PPT Presentation
Variability of the Atlantic North Equatorial Countercurrent NECC - Variability of the Atlantic North Equatorial Countercurrent (NECC) ... Mean dif=-2m mean rms dif=7m. Mean dif=-3m mean rms dif=8m. PIRATA MEETING, MIAMI 2006 ...
Variability of the Atlantic North Equatorial Countercurrent (NECC) ... Mean dif=-2m mean rms dif=7m. Mean dif=-3m mean rms dif=8m. PIRATA MEETING, MIAMI 2006 ...
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Meso- - Scale and Meso- -Scale Convective Systems PowerPoint PPT Presentation
Meso- - Scale and Meso- -Scale Convective Systems - Meso- - Scale and Meso- -Scale Convective Systems
Meso- - Scale and Meso- -Scale Convective Systems
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Incorporation of dynamic balance in data assimilation and application to coastal ocean PowerPoint PPT Presentation
Incorporation of dynamic balance in data assimilation and application to coastal ocean - Incorporation of dynamic balance in data assimilation and application to coastal ocean
Incorporation of dynamic balance in data assimilation and application to coastal ocean
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Day 1 Diagnosis PowerPoint PPT Presentation
Day 1 Diagnosis - http://www.crh.noaa.gov/arx/micrope.html. Precipitation type ... This workshop linked to. http://www.wdtb.noaa.gov. Precipitation efficiency ...
http://www.crh.noaa.gov/arx/micrope.html. Precipitation type ... This workshop linked to. http://www.wdtb.noaa.gov. Precipitation efficiency ...
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Status of Hybrid DWL Study PowerPoint PPT Presentation
Status of Hybrid DWL Study - Independent evaluation and comparative cost analyses ... http://nais.msfc.nasa.gov/cgi-bin/EPS/synopsis.cgi?acqid=99220. JEM/CDL. Scaling TODWL ...
Independent evaluation and comparative cost analyses ... http://nais.msfc.nasa.gov/cgi-bin/EPS/synopsis.cgi?acqid=99220. JEM/CDL. Scaling TODWL ...
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Regional%20Coastal%20Ocean%20Modeling:%20Forcing PowerPoint PPT Presentation
Regional%20Coastal%20Ocean%20Modeling:%20Forcing - Regional Coastal Ocean Modeling: Forcing
Regional Coastal Ocean Modeling: Forcing
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ATMS 316 Mesoscale Meteorology PowerPoint PPT Presentation
ATMS 316 Mesoscale Meteorology - Gulf of Alaska. Autumn of 1980 ... .com/images/maps/map1003.gif. Introduction ... Short trough-ridge spacing large positive vorticity advection above sfc front ...
Gulf of Alaska. Autumn of 1980 ... .com/images/maps/map1003.gif. Introduction ... Short trough-ridge spacing large positive vorticity advection above sfc front ...
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A Climatological Perspective of the 1962 Columbus Day Storm PowerPoint PPT Presentation
A Climatological Perspective of the 1962 Columbus Day Storm - A Climatological Perspective of the 1962 Columbus Day Storm Wolf Read PhD Candidate Forest Science University of British Columbia wolfread@alumni.ubc.ca
A Climatological Perspective of the 1962 Columbus Day Storm Wolf Read PhD Candidate Forest Science University of British Columbia wolfread@alumni.ubc.ca
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mcgill freezing rain PowerPoint PPT Presentation
mcgill freezing rain - 2.) Consider model representation of these processes. 3.) Update you on status of model improvements ... Also: Mike Brennan, Al Riordan (NCSU), Greg Fishel (WRAL) ...
2.) Consider model representation of these processes. 3.) Update you on status of model improvements ... Also: Mike Brennan, Al Riordan (NCSU), Greg Fishel (WRAL) ...
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Nares Strait Atmospheric Modeling PowerPoint PPT Presentation
Nares Strait Atmospheric Modeling - 41-mb along the Strait! ... Evidence for atmospheric control of sea-ice motion through Nares Strait. ... Nares Strait ice flux (GRL, 2006) Analysis of model ...
41-mb along the Strait! ... Evidence for atmospheric control of sea-ice motion through Nares Strait. ... Nares Strait ice flux (GRL, 2006) Analysis of model ...
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QG Dynamics PowerPoint PPT Presentation
QG Dynamics - QG Dynamics A Review Anthony R. Lupo Department of Soil, Environmental, and Atmospheric Science 302 E ABNR Building University of Missouri Columbia, MO 65211
QG Dynamics A Review Anthony R. Lupo Department of Soil, Environmental, and Atmospheric Science 302 E ABNR Building University of Missouri Columbia, MO 65211
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Formation PowerPoint PPT Presentation
Formation - 1997 : CANARI replaced by 3D-VAR at MF (CANARI quality control and surface analysis kept) ... NAIMPO: controls some observations related prints ...
1997 : CANARI replaced by 3D-VAR at MF (CANARI quality control and surface analysis kept) ... NAIMPO: controls some observations related prints ...
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An Extended CAD Spectrum PowerPoint PPT Presentation
An Extended CAD Spectrum - Review CAD detection algorithm and climatology. Review workings of algorithm ... Classical (dry onset) minus Classical (diab. enhanced) Conclusions, & the Next Step ...
Review CAD detection algorithm and climatology. Review workings of algorithm ... Classical (dry onset) minus Classical (diab. enhanced) Conclusions, & the Next Step ...
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PREDICTION OF FRONTOGENETICALLY FORCED PRECIPITATION BANDS PowerPoint PPT Presentation
PREDICTION OF FRONTOGENETICALLY FORCED PRECIPITATION BANDS - PREDICTION OF FRONTOGENETICALLY FORCED PRECIPITATION BANDS. PETER C. BANACOS ... Corresponds to vertical motion on the frontal scale (mesoscale bands) ...
PREDICTION OF FRONTOGENETICALLY FORCED PRECIPITATION BANDS. PETER C. BANACOS ... Corresponds to vertical motion on the frontal scale (mesoscale bands) ...
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Unidata software and data usage at University of Wisconsin Madison PowerPoint PPT Presentation
Unidata software and data usage at University of Wisconsin Madison - Advection terms move EKE around but do not create or destroy it. GFS Energetics plots ... of EKE due to eddy advection. GFS Energetics plots. Steven Decker ...
Advection terms move EKE around but do not create or destroy it. GFS Energetics plots ... of EKE due to eddy advection. GFS Energetics plots. Steven Decker ...
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Seasonal, Interannual, and Decadal Scale Freshwater Variability PowerPoint PPT Presentation
Seasonal, Interannual, and Decadal Scale Freshwater Variability - 1 Institute of Marine Science, University of Alaska, Fairbanks, AK 99709 ... Spall, M. A. and D. C. Chapman, On the efficiency of baroclinic eddy heat ...
1 Institute of Marine Science, University of Alaska, Fairbanks, AK 99709 ... Spall, M. A. and D. C. Chapman, On the efficiency of baroclinic eddy heat ...
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Importance of Winds for Climate and Stratospheric Processes PowerPoint PPT Presentation
Importance of Winds for Climate and Stratospheric Processes - Circumpolar flow and Southern Hemisphere climate change (Thompson and Solomon, 2002) ... characterized by fluctuations in the strength of the circumpolar vortex ...
Circumpolar flow and Southern Hemisphere climate change (Thompson and Solomon, 2002) ... characterized by fluctuations in the strength of the circumpolar vortex ...
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Numerical Simulations of the Extratropical Transition of Floyd 1999: Structural Evolution and Respon PowerPoint PPT Presentation
Numerical Simulations of the Extratropical Transition of Floyd 1999: Structural Evolution and Respon - The Miller (1948) frontogenesis equation was calculated on pressure levels. The scalar frontogenesis, which is defined as the Lagrangian rate of change of ...
The Miller (1948) frontogenesis equation was calculated on pressure levels. The scalar frontogenesis, which is defined as the Lagrangian rate of change of ...
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A variational data assimilation system for the global ocean PowerPoint PPT Presentation
A variational data assimilation system for the global ocean - A variational data assimilation system for the global ocean ... Global (ORCA): 2o x 0.5o at eq., 31 levels (free surface) Variational assimilation environment ...
A variational data assimilation system for the global ocean ... Global (ORCA): 2o x 0.5o at eq., 31 levels (free surface) Variational assimilation environment ...
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Introduction to Mesoscale Meteorology PowerPoint PPT Presentation
Introduction to Mesoscale Meteorology - Geostrophic (Horizontal Pressure Gradient versus vertical Coriolis effect) ... Simple model: Quasi-Geostrophic model: positive vorticity advection results in ...
Geostrophic (Horizontal Pressure Gradient versus vertical Coriolis effect) ... Simple model: Quasi-Geostrophic model: positive vorticity advection results in ...
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midterm 2006 PowerPoint PPT Presentation
midterm 2006 - ... in northern Italy, on the south side of the Alps, it also tends to ... with cold air pouring south west of the Alps, and a pocket of warm air remaining ...
... in northern Italy, on the south side of the Alps, it also tends to ... with cold air pouring south west of the Alps, and a pocket of warm air remaining ...
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On Mesoscale Vortex Rossby Wave in Zonal Shear Flow PowerPoint PPT Presentation
On Mesoscale Vortex Rossby Wave in Zonal Shear Flow - On Mesoscale Vortex Rossby Wave in Zonal Shear Flow. Xinyong Shen ... Nanjing University of Information Science and Technology, Nanjing, China ...
On Mesoscale Vortex Rossby Wave in Zonal Shear Flow. Xinyong Shen ... Nanjing University of Information Science and Technology, Nanjing, China ...
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Numerical Weather Prediction Parameterization of diabatic processes Convection IV Forecasting and Di PowerPoint PPT Presentation
Numerical Weather Prediction Parameterization of diabatic processes Convection IV Forecasting and Di - Numerical Weather Prediction Parameterization of diabatic processes Convection IV Forecasting and Di
Numerical Weather Prediction Parameterization of diabatic processes Convection IV Forecasting and Di
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Ensemble filter data assimilation: Application to probabilistic nowcasting of boundary layer profile PowerPoint PPT Presentation
Ensemble filter data assimilation: Application to probabilistic nowcasting of boundary layer profile - Advection and radiation play roles at different heights. Assimilation-advection synergism ... Advection has often a positive effect as it brings 3D dynamics. ...
Advection and radiation play roles at different heights. Assimilation-advection synergism ... Advection has often a positive effect as it brings 3D dynamics. ...
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Lectures on Modeling and Data Assimilation PowerPoint PPT Presentation
Lectures on Modeling and Data Assimilation - Lectures on Modeling and Data Assimilation Richard B. Rood NASA/Goddard Space Flight System Visiting Scientist, Lawrence Livermore National Laboratory
Lectures on Modeling and Data Assimilation Richard B. Rood NASA/Goddard Space Flight System Visiting Scientist, Lawrence Livermore National Laboratory
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How to Use an 500Mb Chart PowerPoint PPT Presentation
How to Use an 500Mb Chart - When forecasters think of the 500-millibar chart one of the top words that comes ... The upper levels of the atmosphere are generally stable with geostrophic flow. ...
When forecasters think of the 500-millibar chart one of the top words that comes ... The upper levels of the atmosphere are generally stable with geostrophic flow. ...
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Numerical Weather Prediction Parametrization of diabatic processes Convection I PowerPoint PPT Presentation
Numerical Weather Prediction Parametrization of diabatic processes Convection I - Numerical Weather Prediction Parametrization of diabatic processes Convection I Peter Bechtold and Christian Jakob Convection Lectures: The nature of convection ...
Numerical Weather Prediction Parametrization of diabatic processes Convection I Peter Bechtold and Christian Jakob Convection Lectures: The nature of convection ...
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