Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss The new algorithm for gridpoint - station correspondence.

Slides:



Advertisements
Similar presentations
Maps and Aerial Photos There are many different kinds of maps Geopolitical Topographic Shaded Relief, Photorectified or Standard Geologic Ecosystemic Meteorological.
Advertisements

5.6 Projectiles Launched at an Angle
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss The Latent Heat Nudging Scheme of COSMO EWGLAM/SRNWP Meeting,
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss WG5-Report from Switzerland: Verification of COSMO in.
Map Projections (1/2) Francisco Olivera, Ph.D., P.E. Center for Research in Water Resources University of Texas at Austin.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Numerical weather prediction from short to long range.
* Reading Assignments:
What else do maps tell us?. Maps tell us where places are located - but they also contain lots more information. What other information does the map provide.
1. A man flies a kite with a 100 foot string
Wind Driven Circulation I: Planetary boundary Layer near the sea surface.
DO NOW Superman is looking for Lois Lane. He starts flying from the roof of the Daily Planet, flies 5km east, 5 km north, 5 km south and 7 km west. He.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss MeteoSwiss acceptance procedure for automatic weather.
Maps and Map Reading.
Finding Areas of Shapes. Area of a Triangle Area of Triangle = 1 x Base x Vertical Height 2 Vertical Height Base Right Angle.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Parametrization of Subgrid-Scale Orographic Drag in the.
2D into 3D Reinterpreting Famous Artworks from History.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss High-resolution data assimilation in COSMO: Status and.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Report on Workshop « Stratified verification by weather.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Data mining in the joint D- PHASE and COPS archive Mathias.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Component testing of the COSMO model’s turbulent diffusion.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Task 1 of PP Interpretation 1.1Further applications of.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss High Resolution Snow Analysis for COSMO
June 19, 2007 GRIDDED MOS STARTS WITH POINT (STATION) MOS STARTS WITH POINT (STATION) MOS –Essentially the same MOS that is in text bulletins –Number and.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Final PP QPF meeting COSMO General Meeting, 18 September.
The Earth © Lisa Michalek.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Stability of the COSMO turbulence scheme Oliver Fuhrer.
Fluid dynamic simulation in the analysis of the microclimate
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Atmosphere at rest experiments with the latest COSMO version.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss High resolution COSMO runs for dispersion applications.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Conditional verification of all COSMO countries: first.
Latest results in verification over Poland Katarzyna Starosta, Joanna Linkowska Institute of Meteorology and Water Management, Warsaw 9th COSMO General.
The latest results of verification over Poland Katarzyna Starosta Joanna Linkowska COSMO General Meeting, Cracow September 2008 Institute of Meteorology.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Priority project « Advanced interpretation and verification.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Postprocessing of temperature and wind for COSMO-7 and.
The climate and climate variability of the wind power resource in the Great Lakes region of the United States Sharon Zhong 1 *, Xiuping Li 1, Xindi Bian.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Verification results of COSMO at MeteoSwiss in the year.
9-3 Angles of Elevation and Depression
Federal Departement of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Revisiting Swiss temperature trends * Paulo.
WRF Four-Dimensional Data Assimilation (FDDA) Jimy Dudhia.
Wind.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Local Probabilistic Weather Predictions for Switzerland.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss WG 4 activities.
Verification Verification with SYNOP, TEMP, and GPS data P. Kaufmann, M. Arpagaus, MeteoSwiss P. Emiliani., E. Veccia., A. Galliani., UGM U. Pflüger, DWD.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Weather types and gridding of daily precipitation in the.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Status of MeteoSwiss 18 September 2008 COSMO GM 2008.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Status of the COSMO-1 configuration at MeteoSwiss Guy.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss TKE as a measure of turbulence COSMO General Meeting,
The correction of initial values of temperature at low model levels Blinov D. Revokatova A. Rivin G. Rozinkina I. Sapuncova E.
Topographical Maps. What is a topographical map?  A detailed map showing physical and cultural features and the elevation, or height, of the land  Elevation.
October 9 th,  Let's look at our first topic under Mapping Skills - Contour Lines.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Component testing of the COSMO model’s turbulent diffusion.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Probabilities from COSMO-2 derived with the neighborhood.
Comparison of LM Verification against Multi Level Aircraft Measurements (MLAs) with LM Verification against Temps Ulrich Pflüger, Deutscher Wetterdienst.
How to Navigate a Set of Field Notes….. First the Jargon… Benchmark Backsight Foresight Height of Instrument Elevation Turning Point Station.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Numerical Weather Prediction at MeteoSwiss 8th of October.
Objective To use angles of elevation and depression to solve problems.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Status of the COSMO-1 configuration at MeteoSwiss Guy.
Newton’s Universal Law of Gravity Every object attracts every other object with a force that is directly proportional to the masses of the objects and.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss VERSUS: Requirements for TEMPs and windprofilers Francis.
The Earth © Lisa Michalek.
Analysis of ground magnetometer coverage
COSMO General Meeting 2009 WG5 Parallel Session 7 September 2009
A. Topographic radiation correction in COSMO: gridscale or subgridscale? B. COSMO-2: convection resolving or convection inhibiting model? Matteo Buzzi.
Finding the Distance Between Two Points.
Finding the Area of Triangles
Objective - To graph ordered pairs.
Some Verification Highlights and Issues in Precipitation Verification
Angles of Elevation and Depression
How do we Adapt?.
Presentation transcript:

Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss The new algorithm for gridpoint - station correspondence Pirmin Kaufmann, MeteoSwiss

2 COSMO General Meeting 2007, Athens, Greece Find grid cell to which station belongs Find grid cell within which station (red star) is located (nearest neighbour: round grid coordinates of station) Determine if cell has land or water surface (water: SOILTYP = 9 or FR_LAND < 50%) land? water?

3 COSMO General Meeting 2007, Athens, Greece Search radius Search radius over land = gp (~  2) Search radius over water = 2 gp Rationale: many stations on small peninsulas are almost 2 gp from the nearest model land point ? ?? ?

4 COSMO General Meeting 2007, Athens, Greece Search within radius If land is found, only consider these cells If only water grid points are within radius, continue with all grid points within radius Rationale Some parameters are quite different over sea and over land (especially temperature) Stations are usually placed on land Some stations are far from any land (e.g. oil rigs in the north sea)

5 COSMO General Meeting 2007, Athens, Greece Optimize horizontal and vertical distance Calculate horizontal distance d hor and vertical distance dz in meter Look for station with smallest „optimization-distance“ according to : Dist = d hor + 500*dz Example: to avoid a vertical distance of 20 m, we allow a horizontal distance up to 10 km x, y z Lines of equal dist

6 COSMO General Meeting 2007, Athens, Greece Advantages Better verification results because height differences of less than 100 m still matter (and sometimes quite a lot) Simple optimization algorithm Avoid using more distant grid point just because of slightly smaller height difference (above 100 m) Avoid using grid point with more height difference (below 100 m) when grid point with smaller height difference is almost as near.

7 COSMO General Meeting 2007, Athens, Greece Summary Find grid cell within which station is located (=round grid coordinates of station) Determine if SOILTYP = 9 (or FR_LAND < 50%) Search radius over water = 2 gp Search radius over land = gp (~  2) Search within this radius If solid ground is found, only consider these cells If only water is found, continue with all cells within radius Calculate horizontal distance d hor and vertical distance dz in meter Look for station with smallest total distance according to Dist = d hor + 500*dz