'Model levels' presentation slideshows

Bring i ng together CMIP5 & CORDEX Data management 8 March 2011, SMHI, Norrkoeping

Bring i ng together CMIP5 & CORDEX Data management 8 March 2011, SMHI, Norrkoeping. Topics. Data management in CORDEX : Get access to CMIP5 global forcing data role of IS-ENES ? CMIP5 formatted data not CMIP5 formatted data Provide access to CORDEX results role of IS-ENES ?

572 views • 43 slides

WRF Physics Options

WRF Physics Options. Jimy Dudhia. diff_opt=1. 2 nd order diffusion on model levels Constant coefficients (khdif and kvdif) km_opt ignored. diff_opt=2. 2 nd order horizontal diffusion Allows for terrain-following coordinate Uses km_opt 1: constant (khdif and kvdif used)

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394 views • 27 slides

349 views • 19 slides

Operational Scheme and Schedule: Basics

Operational Scheme and Schedule: Basics. Basic scheme (analysis + forecast) Global-Modell (GME, global and synoptic-scale) Lokal Modell (LM, highly resolved mesoscale model) 3 runs per day 00, 12, 18 UTC 03, 06, 09, 15, 21 UTC only analysis Schedule determined by data cut-off

280 views • 18 slides

VERSUS: Requirements for TEMPs and windprofilers Francis Schubiger & Christophe Hug MeteoSwiss

VERSUS: Requirements for TEMPs and windprofilers Francis Schubiger & Christophe Hug MeteoSwiss. VERSUS meeting Langen (D), 4 March 2010. Requirements for TEMPs verification (1). Verification: for all 12h (wind alone also for all 6h) starting at +0h at surface and on the following p-levels:

294 views • 18 slides

TR AZOMOZA IC Comparison in the UTLS

TR AZOMOZA IC Comparison in the UTLS. Andreas Volz-Thomas and Martin G. Schultz. Uncertainties in the Global Tropospheric Ozone Budget. Objectives. Analyse observed and simulated trace gas concentrations relative to the tropopause

276 views • 16 slides

Reasoning for Microphysics Modifications

Reasoning for Microphysics Modifications . Several modification were made to Thompson microphysics schemes: Changes to homogeneous freezing temperature (HGFR) from 235 to 271 K Desired effect of changing liquid clouds to ice clouds

241 views • 11 slides

Model Vertical Coordinates and Levels and Nesting

Model Vertical Coordinates and Levels and Nesting. Model Vertical Coordinates. Earliest models were in z or p. A problem near terrain (complex boundary conditions where model level intersected mountains)

113 views • 11 slides

Model Vertical Coordinates and Levels and Nesting

Model Vertical Coordinates and Levels and Nesting. Model Vertical Coordinates. Earliest models were in z or p. A problem near terrain (complex boundary conditions where model level intersected mountains)

111 views • 11 slides

Terrain-mapped Cross Sections in MATLAB

Terrain-mapped Cross Sections in MATLAB. Erik Neemann 15 April 2014. Objective. Create cross sections visually similar to what is produced in RIP Add capability to plot time-averaged data. Before. After. Notes. Code built to produce cross section of zonal wind component in Uintah Basin

232 views • 8 slides

Interesting Papers of EDOC 2013

Interesting Papers of EDOC 2013. by Matt Selway KSE Lab Meeting 10 Dec 2013. Introduction. EDOC 2013 The Enterprise Computing Conference Covers diverse areas of enterprise computing including: Enterprise architecture Services, SoA Model-based approaches Business processes etc.

203 views • 7 slides