January 29-30, 2013 simulated composite reflectivity (dBZ).January 29-30, 2013 simulated surface equivalent potential temperature (K) and winds (m/s).

Slides:



Advertisements
Similar presentations
Lapse Rate is the temperature drop per kilometer height increase Typically about 6 °C/km = 6 °C/1000m Or About 3 °F/1000 ft.
Advertisements

If θ/z = 0, the atmosphere is said to be neutral,or neutrally stratified, and the lapse rate is equal to the dry adiabatic lapse rate (DALR) Γ d ~= 10.
Michael B. McElroy ACS August 23rd, 2010.
Solutions to Chapter 3 Assignment 3 CE/AE/EnvSci 4/524.
Cold Fronts and their relationship to density currents: A case study and idealised modelling experiments Victoria Sinclair University of HelsinkI David.
38 Atmospheric Stability Stable vs. Unstable Dry and Moist Adiabatic Processes Skew-T diagrams.
Skew-T Thermodynamic Diagram Global distribution of weather balloon stations.
Skew T. What is a skew-T diagram? Diagram used to plot vertical profiles through the atmosphere Determine atmospheric stability.
Dynamical Downscaling of CCSM Using WRF Yang Gao 1, Joshua S. Fu 1, Yun-Fat Lam 1, John Drake 1, Kate Evans 2 1 University of Tennessee, USA 2 Oak Ridge.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 2 “The atmosphere (II)” Dr. Eugene Cordero San Jose State University.
300 hPa height (solid, dam), wind speed (shaded, m s −1 ), 300 hPa divergence (negative values dashed, 10 −6 s −1 ) n = 22 MSLP (solid, hPa),
Bow Echo Sensitivity to Ambient Moisture and Cold Pool Strength Richard P. James, Paul M. Markowski, and J. Michael Fritsch, 2006: Mon. Wea. Rev., 134,
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.
A M ULTISCALE A NALYSIS OF A H EAVY R AINFALL E VENT OVER L AKE M ICHIGAN Jason M. Cordeira D EPARTMENT OF A TMOSPHERIC AND E NVIRONMENTAL S CIENCES U.
THE BLACK FOREST STORM OF 15 JULY 2007: NUMERICAL SIMULATION AND SENSITIVITY STUDIES Evelyne Richard 1, Jean-Pierre Chaboureau 1 Cyrille Flamant 2 and.
Hector simulation We found simulation largely depending on: Model initialization scheme Lateral boundary conditions Physical processes represented in the.
Annual-mean TOA radiation (ERBE, W/m 2 ) Absorbed SW Outgoing LW.
* Reading Assignments:
Chris Birchfield Atmospheric Sciences, Spanish minor.
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Atmospheric Moisture Vapor pressure (e, Pa) The partial pressure exerted by the molecules of vapor in the air. Saturation vapor pressure (e s, Pa ) The.
Moisture Moisture = Water Vapor (gas) Gets into the atmosphere by: 1.Evaporation = liquid to gas (opposite of condensation) 2.Transpiration = plants release.
EFFECT OF SALINITY ON FREEZING AND DENSITY OF WATER.
Squall Lines moving over Santarem Julia Cohen Federal University of Para, Brazil David Fitzjarrald Atmospheric Sciences Research Center/ University at.
II. Changes Between Liquid and Gas Vaporization: The change in state from liquid to gas. Vaporization.
Comparison of Evaporation and Cold Pool Development between Single- Moment (SM) and Multi-moment (MM) Bulk Microphysics Schemes In Idealized Simulations.
赴国际水稻所访学情况汇报 长江大学农学院 邢丹英 2010 年 6 月. 学习目的 学习时间、地点 学习内容 学习收获 几点体会 汇报提纲.
ATMOSPHERE HEATING RATE: CLOUD FREE ATMOSPHERE. Words and Equation from Petty: Radiative Heating Rate.
Three Lectures on Tropical Cyclones Kerry Emanuel Massachusetts Institute of Technology Spring School on Fluid Mechanics of Environmental Hazards.
1 Scott Zaccheo AER, Inc ASCENDS End-to-End System Performance Assessment: Analysis of Atmospheric State Vector Variability.
Chapter 7: convective initiation
A Contrast of Two Las Vegas Flash Flood Scenarios Introduction/BackgroundIntroduction/Background A Classic Monsoon CaseA Classic Monsoon Case »July 8,
Thermal comfort PMV: predicted mean vote. M: metabolism (W/m2).
Meng, Z., F. Zhang, P. Markoswki, D. Wu, and K. Zhao, 2012: A modeling study on the development of a bowing structure and associated rear inflow within.
Unit 4 Vocabulary The Atmosphere. 1. Storm surge – abnormal rise of the sea along a shore as a result of strong winds 2. local winds – winds causes by.
RESOURCES & ENVIRONMENT CH. 4. SOLAR ENERGY
INTERPRETING A SKEW-T LOG-P AEROLOGICAL DIAGRAM
A JUNE MONSOON? David L. Mitchell 1, Dorothea Ivanova 1 and David Gochis 2 1.Desert Research Institute, Reno, Nevada 2. National Center for Atmospheric.
Exercise1 You will find; 1.Fog / Stratiform Cloud 2.Cb / Cg 3.Transverse Line 4.Upper level flow 5.Jet stream, upper level vortex… 6.Lower level flow 7.Tropical.
Chapter 7: convective initiation squall line development in Illinois a visible satellite image loop of CI in the eastern US 35°N 103°W Fig. 7.2.
南水北调东线第一期工程山东段 情况简介. 主要汇报内容 二、南水北调山东段工程总体布置 三、山东段工程项目划分及工程主 要建设内容 一、南水北调东线工程概况 四、前期工作及工程建设进展情况 五、工程总投资.
SCSL SWAP/LYRA workshop
Description of the climate system and of its components
Equivalent Ratios.
The May 24 Shamrock cold front
Hyperspectral Wind Retrievals Dave Santek Chris Velden CIMSS Madison, Wisconsin 5th Workshop on Hyperspectral Science 8 June 2005.
Structure of the atmosphere
Impact of Assimilated Boundary Conditions on WRF-NMM/CMAQ Air Quality Predictions Researchers at NESDIS, NCEP and the NWS used global ozone analyses from.
Lapse Rate Poisson equation: d ( ).
ATOC 4720: class 6: Winds and precipitation
Hosted by Ms. Vaughn.
Hosted by Ms. Vaughn.
Nonlinear modulation of O3 and CO induced by mountain waves in the UTLS region during TREX Mohamed Moustaoui(1), Alex Mahalov(1), Hector Teitelbaum(2)
Hosted by Ms. Vaughn.
1. Transformations of Moist Air
Climate.
Deep Circulation Changes in density cause ocean currents Cold Warm
Hosted by Ms. Vaughn.
Course IIA1117 Control Engineering Fall 2018 Ratio control
Course IIA1117 Control Engineering Fall 2017 Ratio control
Hosted by Ms. Vaughn.
Hosted by Ms. Vaughn.
Ratio: Equivalent ratio
Changes in State Chapter 8 - Lesson 2 pages
REGIONAL AND LOCAL-SCALE EVALUATION OF 2002 MM5 METEOROLOGICAL FIELDS FOR VARIOUS AIR QUALITY MODELING APPLICATIONS Pat Dolwick*, U.S. EPA, RTP, NC, USA.
Fundamental Eqs for modeling clouds
Fraction of BaP remaining in an 8-nm-thick cooking oil film exposed to different gas-phase ozone mixing ratios after 1 h (black), 12 h (purple), 1 d (blue),
CHAPTER 3 LESSON 2 SYSTEM INTERACTIONS.
Hosted by Ms. Vaughn.
Presentation transcript:

January 29-30, 2013 simulated composite reflectivity (dBZ).January 29-30, 2013 simulated surface equivalent potential temperature (K) and winds (m/s).

Boundary-relative surface-based CAPE for 7 points (black dashed) and the 7 point average (red). Boundary-relative surface potential temperature for 7 points (black dashed) and the 7 point average (red).

Boundary-relative surface water vapor mixing ratio for 7 points (black dashed) and the 7 point average (red). Boundary-relative km lapse rates for 7 points (black dashed) and the 7 point average (red).