Sea Level Pressure for the max – min Eurasian experiment

Slides:



Advertisements
Similar presentations
If R = {(x,y)| y = 3x + 2}, then R -1 = (1) x = 3y + 2 (2) y = (x – 2)/3 (3) {(x,y)| y = 3x + 2} (4) {(x,y)| y = (x – 2)/3} (5) {(x,y)| y – 2 = 3x} (6)
Advertisements

Extreme cold events over Asia: role of stratospheric wave reflection By Debashis Nath & Chen WEN International Workshop on High Impact weather Research.
Seasonal to decadal prediction of the Arctic Oscillation D. Smith, A. Scaife, A. Arribas, E. Blockley, A. Brookshaw, R.T. Clark, N. Dunstone, R. Eade,
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Modeled response of snow cover- atmosphere-ocean interactions in the Northern Hemisphere. Gina Henderson, Daniel J. Leathers and Brian Hanson Department.
Project Maths - Teaching and Learning Relative Frequency % Bar Chart to Relative Frequency Bar Chart What is the median height.
Recitation Geostrophic Balance Thermal Wind Effect of Friction.
Annual- and zonal-mean climate of the tropics (NCEP) Relative humidity [%] Temperature [degC] surface pressure [mb] equatorial trough subtropical high.
Fig. 1. NCEP/NCAR Composite analysis 24 hours prior to event onset (T-24) for a) 250-hPa vector wind, b) 500-hPa geopotential height, c) 850-hPa temperature,
Ross Wagenseil for CDMP January 2000 N Wind Wave Surge 10yr25yr50yr100yr SELECT Points of Interest: MILES KILOMETERS ARC-MINUTES 0 5.
A comparison of North Atlantic storms in HiGEM, HadGEM and ERA-40 Jennifer Catto – University of Reading Supervisors: Len Shaffrey Warwick Norton Acknowledgement:
El Niño, La Niña and ENSO La NiñaEl Niño Time mean.
Ozone Observations Analyses on Eastern Island La Serena, 22 Nov Juan Quintana Dirección Meteorológica de Chile
5.7 PW5.9 PW The seasonal cycle of energy fluxes in the high latitudes Aaron Donohoe I.) How do the absorbed solar (ASR), outgoing longwave (OLR), and.
1 The BD circulation and wave forcing Influence on the QBO period Le Kuai.
GFS (green), ECMWF (blue) 500 mb height 00 hr forecasts 12z 24 Dec
GDAS analysis 500 mb height/absolute vorticity 00z 24 Dec 2010.
General Circulation of the Atmosphere Lisa Goddard 19 September 2006.

A Decline in the Northern Hemisphere CO 2 Sink from John Miller 1, Pieter Tans 1, Jim White 2, Ken Masarie 1, Tom Conway 1, Bruce Vaughn 2,
Monsoons. Monsoon Flow Patterns (Figure obtained from Introduction to Tropical Meteorology, 2 nd Edition, © 2011 COMET.)
Self-organizing maps (SOMs) and k-means clustering: Part 2 Steven Feldstein The Pennsylvania State University Trieste, Italy, October 21, 2013 Collaborators:
Wintertime climate variations forced by changes in earth’s orbit Alex Hall UCLA Dep’t of Atmospheric and Oceanic Sciences Amy Clement Rosenstiel School.
ENSO impact to atmospheric circulation system for summer Motoaki Takekawa Tokyo Climate Center, Japan Meteorological Agency (JMA) 1.
Paper review Speaker : Pei-Yu Chueh Adviser : Yu-Heng Tseng Date : 2011/3/22.
Extra-tropical climate and the modelling of the stratosphere in coupled atmosphere ocean models. E Manzini Istituto Nazionale di Geofisica e Vulcanologia.
EVAT 554 OCEAN-ATMOSPHERE DYNAMICS FILTERING OF EQUATIONS FOR OCEAN LECTURE 10 (Reference: Peixoto & Oort, Chapter 3,8)
NOAA's 33rd Climate Diagnostics and Prediction Workshop/CLIVAR Drought Workshop (CDPW) October 20-24, 2008 in Lincoln, Nebraska Hydrodynamics of the Caribbean.
Diagnostics, Special Projects and Phenomena of Interest Review of 2 nd C20C Workshop for 3 rd C20C Workshop ICTP, Trieste, Italy, 21 April 2004.
The Linear and Non-linear Evolution Mechanism of Mesoscale Vortex Disturbances in Winter Over Western Japan Sea Yasumitsu MAEJIMA and Keita IGA (Ocean.
Lecture 5: Wind & effects of friction. The atmosphere is warmer in the equatorial belt than over the polar caps. These horizontal temperature gradients.
Aircraft, Satellite Measurements and Numerical Simulations of Gravity Waves in the Extra-tropical UTLS Region Meng Zhang, Fuqing Zhang and Gang Ko Penn.
EVAT 554 OCEAN-ATMOSPHERE DYNAMICS EQUATIONS OF MOTION (CONT); ENERGY EQUATION LECTURE 4 (Reference: Peixoto & Oort, Chapter 3)
INTRODUCTION DATA SELECTED RESULTS HYDROLOGIC CYCLE FUTURE WORK REFERENCES Land Ice Ocean x1°, x3° Land T85,T42,T31 Atmosphere T85,T42,T x 2.8 Sea.
PAPER REVIEW R Kirsten Feng. Impact of global warming on the East Asian winter monsoon revealed by nine coupled atmosphere-ocean GCMs Masatake.
Points of Interest: Ross Wagenseil for CDMP January 2000 CDMP 10.9 N 61.0 W N W The projection of the illustrations is Plate Carrée, a square.
MARINE ECOSYSTEMS GEOL 1033 (Lesson 36) ppt file b.
Climate-Weather Presentation For Climate Modeling 11 September 2015.
OUTLINE Examples of AMOC variability and its potential predictability, Why we care, Characteristics of AMOC variability in a CCSM3 present-day control.
Ippolitov I. I., Kabanov M. V., Komarov A. I., Kuskov A. I., Loginov S. V., Smirnov S. V. Structure and Dynamics of Ground Temperature and Pressure Fields.
Paper Review R 馮培寧 Kirsten Feng. The North Pacific Oscillation – West Pacific Teleconnection Pattern : Mature-Phase Structure and Winter Impacts.
Changes in Sea Ice Alison Liou Meghan Goodwin. Arctic Oscillation (Northern Annular Mode) Antarctic Oscillation (Southern Annular Mode) Zonal = movement.
Points of Interest: Ross Wagenseil for CDMP January 2000 CDMP 16.5 N W 17.0 N W The projection of the illustrations is Plate Carrée, a square.
Height Matters. Wind, Temperature, and Humidity.
The Atmospheric Response to Changes in Tropical Sea Surface Temperatures An overview of Gill, A.E., 1980, Some simple solutions for heat- induced tropical.
Fig Wilkins Ice Shelf breakup events of (a) MODIS band 1 image 10 days after the end of the first event; (b) Envisat ASARimage during the second.
Monsoons. Monsoon Flow Patterns (Figure obtained from Introduction to Tropical Meteorology, 2 nd Edition, © 2011 COMET.)
Oliver Elison Timm ATM 306 Fall 2016
Paper Review Kirsten Feng.
Dominica Probable Storm Effects Points of Interest: Dominica
The Experimental Climate Prediction Center Regional Spectral Model (ECPC-RSM) Contribution to the North American Regional Climate Change Assessment Program.
Question 1 height of the 1000 hPa surface pressure (Pa) at sea level.
A-DRY Heatles adsorption compressed air dryer Simulation
St. Vincent Probable Storm Effects Points of Interest: St. Vincent
TALLEY Copyright © 2011 Elsevier Inc. All rights reserved
The West Coast Thermal Trough
MDI Global Field & Solar Wind
Max 5yr snow.
Monsoons.
Non rotating planet.
Non rotating planet.
Climatological mean features and interannual to decadal variability of ring formations in the Kuroshio Extension.
D1 D2 D3 D4 Figure 2 Initial sea-surface temperature (SST, color) and ocean heat content (OHC, contour) fields for the coupled model simulation of Hurricane.
Hadley Cell.
Homework Analyzing Graphs
Toward a better understanding of the natural climatic variability
500 hPa height , surface pressure
Scott A. Braun, 2002: Mon. Wea. Rev.,130,
Sec 4.3: HOW DERIVATIVES AFFECT THE SHAPE OF A GRAPH
Ryan L. Fogt Department of Geography Ohio University, Athens, OH
Presentation transcript:

Sea Level Pressure for the max – min Eurasian experiment With SOM With DOM

500 hPa Heights for the max – min Eurasian experiment With SOM With DOM

Meridional Flux of Zonal Momentum for the max – min Eurasian experiment With SOM With DOM

Sea Level Pressure for the max – min North American experiment With SOM With DOM

500 hPa Heights for the max – min North American experiment With SOM With DOM

Meridional Flux of Zonal Momentum for the max – min North American experiment With SOM With DOM