'Mean sea level pressure' diaporamas de présentation

Upper Air and Soundings

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UM 4D-Var Regional Reanalysis Progress

UM 4D-Var Regional Reanalysis Progress. Richard Renshaw, Stephen Oxley, Adam Maycock, Peter Jermey, Dale Barker, DingMin Li. Contents. Progress with technical work First attempt at reanalysis Developments for 2012/13. WP2.1 Building capacity for advanced regional data assimilation.

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Climate Change Teleconnections AO, NAO, ENSO, PDO

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Statistical Projection of Global Climate Change Scenarios onto Hawaiian Rainfall

Statistical Projection of Global Climate Change Scenarios onto Hawaiian Rainfall. Oliver Timm, International Pacific Research Center, SOEST, University of Hawai'i at Manoa Henry Diaz, NOAA/ESRL/CIRES, Boulder, Colorado. Climate Change in the News .

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Section 03 - Altimetry Lesson 08

Section 03 - Altimetry Lesson 08. The Altimeter Altimeter Errors Altimeter Definitions Altimeter Settings. The Altimeter. Close connection between pressure and height It is primarily an instrument merely for measuring pressure. Similar to an aneroid barometer. The Altimeter.

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Forecast sensitivity to observation: Equations

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Introducing the Lokal-Modell LME at the German Weather Service

Introducing the Lokal-Modell LME at the German Weather Service. Jan-Peter Schulz Deutscher Wetterdienst COSMO General Meeting 2005. The expansion of the LM domain has been requested by the following (internal) DWD customers:. LME: LM Europe. Aviation consulting Sea traffic consulting

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Verification of ALADIN/Portugal forecasts

Verification of ALADIN/Portugal forecasts. Margarida Belo (Instituto de Meteorologia, Portugal ). >1550m. >1250m. >300m. ALADIN Orography and portuguese stations. Wind speed (10m). 06UTC. 00UTC. RMSE . 18UTC. Inland (north and center of Portugal). 12UTC.

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Freezing rain event 14-15 December 2005 Central South Carolina

Freezing rain event 14-15 December 2005 Central South Carolina. Tony Petrolito NWS Forecast Office Columbia SC. Introduction. Initially it appeared temperatures would be just warm enough for all rain. Cold dry high pressure to the north.

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Dust modeling with GEOS-Chem: evidence for acidic uptake on dust surfaces during INTEX-B

Dust modeling with GEOS-Chem: evidence for acidic uptake on dust surfaces during INTEX-B. T. Duncan Fairlie NASA Langley Research Center Hampton, Virginia t.d.fairlie@nasa.gov.

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A Climatology of the Convective System Morphology over Northeast United States

A Climatology of the Convective System Morphology over Northeast United States Kelly Lombardo & Brian Colle School of Marine and Atmospheric Sciences Stony Brook University. (m). dBZ. Convective Structures IC: Isolated Cells CC: Cluster of Cells BL: Broken Line NS: No Stratiform

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Cyclone composites in the real world and ACCESS

Cyclone composites in the real world and ACCESS. Pallavi Govekar, Christian Jakob, Michael Reeder and Jennifer Catto. Introduction. The energy budget of the southern hemisphere is poorly represented in nearly all climate models (Trenberth and Fasullo, 2010), with

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DATA and TAPE OUTLAY FOR CFSRR Suru Saha and Patrick Tripp, CFSRR Project, EMC/NCEP 2008 Reanalysis: 1238 Tapes (867

DATA and TAPE OUTLAY FOR CFSRR Suru Saha and Patrick Tripp, CFSRR Project, EMC/NCEP 2008 Reanalysis: 1238 Tapes (867 TB) 2009 Reforecast: 3651 Tapes (2.55 PB) Total: 4889 Tapes (3.4 PB). EXPLANATION OF FILE NAMES Siganl : 3-D Hybrid Analysis (Binary)

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Exam 3 Thursday Nov. 18.

Exam 3 Thursday Nov. 18. . This exam will cover the following chapters in the text book Chapter 8 Pressure and Wind Chapter 9 Small Scale and Local System Chapter 10 Global System Chapter 11 Air Mass and Fronts The corresponding lectures are: Lectures 12 through 16. To prepare:

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