MODEL WIND FIELD COMPARE WITH HRD WIND FIELD

Slides:



Advertisements
Similar presentations
High-Resolution Land Use Data in WPS/WRF for Urban Regions
Advertisements

1 High resolution SST products for 2001 Satellite SST products and coverage In situ observations, coverage Quality control procedures Satellite error statistics.
IFREMER EMPIRICAL ROUGHNESS MODEL Joe Tenerelli, CLS, Brest, France, November 4, 2010.
Choose your characters and drag them onto the slide Write your story title here Story by.
First Category Second Category Third Category Fourth Category $100$200$300$100 $200 $300.
Copyright © 2003 Pearson Education, Inc. Slide Radian Measure, Arc Length, and Area Another way to measure angles is using what is called radians.
Table of Contents Function: Domain and Range A function is a correspondence between two sets governed by some rule(s) such that each member of the first.
Bell Ringer {y>-4} All Real Numbers Domain: Range:
13th EMS & 11th ECAM Model and scatterometer sea surface winds for storm surge applications in the Adriatic Sea Francesco De Biasio*, Stefano Zecchetto,
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.
MMS - Ozonesonde Wind and Temperature Comparison during CR-AVE T.P. Bui, J. Dean-Day, C. Chang, R. Castaneda NASA-Ames Research Center H. Voemel University.
Write your story title here Choose your characters and drag them onto the slide Story by.
Lateral boundary conditions and forecast errors in the mid-latitudes – first results Luka Honzak, Nedjeljka Žagar, Gregor Skok CE Space-SI and University.
TEMPLATE DESIGN © A high-order accurate and monotonic advection scheme is used as a local interpolator to redistribute.
CIMMSE TC Wind Group Conference Call Wednesday, April 10 th, AM.
High Quality Wind Retrievals for Hurricanes Using the SeaWinds Scatterometer W. Linwood Jones and Ian Adams Central Florida Remote Sensing Lab Univ. of.
Comparing initial large-scale fields from two HWRF runs with GFS analysis --Two HWRF configurations ❶ H14C : GSI is used on Domain 1 ❷ T14C: GSI is not.
Coastal Ocean Processes: Homework 1.Investigate what happens if the western side is extended to include a deep (H=1000m) SCS basin: (a) extend as shown;
Problem 3.2. Step One Draw a 4 X 6 rectangle on grid paper and cut it out.
Errors on SMOS retrieved SSS and their dependency to a priori wind speed X. Yin 1, J. Boutin 1, J. Vergely 2, P. Spurgeon 3, and F. Gaillard 4 1. LOCEAN.
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.
Global predictors of regression fidelity A single number to characterize the overall quality of the surrogate. Equivalence measures –Coefficient of multiple.
Where do volcanoes and earthquakes happen?
Trainers name(s) here.
Servo-Finger Linkage as Parallelogram
Kazushi Takemura, Ishioka Keiichi, Shoichi Shige
Verifying Precipitation Events Using Composite Statistics
Coupled atmosphere-ocean simulation on hurricane forecast
continued on next slide
IMPROVING HURRICANE INTENSITY FORECASTS IN A MESOSCALE MODEL VIA MICROPHYSICAL PARAMETERIZATION METHODS By Cerese Albers & Dr. TN Krishnamurti- FSU Dept.
Precision Ag Workshop – Day 1 (RHS00_1.ppt)
What temporal averaging period is appropriate for MM5 verification?
WIND TURBINE GENERATORS.
                                                                                                                                                                                                                                                
continued on next slide
continued on next slide
دفتر برنامه ریزی و کنترل برنامه ها مصطفایی
You control discretization on the Domain pane.
Choose your characters and drag them onto the slide
פחת ורווח הון סוגיות מיוחדות תהילה ששון עו"ד (רו"ח) ספטמבר 2015
Choose your characters and drag them onto the slide
Chapter 3 “Scientific Measurement”
Lidia Cucurull, NCEP/JCSDA
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Runoff Simulations in Region12 (or almost the State of Texas)
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
What happens when we divide fractions?
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
University of Pennsylvania, 1945 (ENIAC museum)
Chebyshev Spectral Method with Domain Decomposition
Choose your characters and drag them onto the slide
The DNSC08ERR Interpolatsion Error
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Question 9.
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
Example Challenge Question
continued on next slide
Types of Errors And Error Analysis.
Choose your characters and drag them onto the slide
Choose your characters and drag them onto the slide
continued on next slide
Presentation transcript:

MODEL WIND FIELD COMPARE WITH HRD WIND FIELD In the second and fourth slide, the model wind field shown here are HRD wind interpolated onto the model domain with 1/12 degree resolution. The resolution for HRD wind is about 6km, which is about 1/20 degree. As you suspected, the model wind field is not exactly equal to HRD wind, the difference are within 2m/s except somewhere on land (lower right corner) and at the center (slide 3, 5). I think what happened is that when I interpolated the HRD wind onto the larger resolution model domain and then interpolate back, it generated errors because of the changing of grid resolution.

Interpolated wind field compare with HRD wind field The slides shown following are comparisons between interpolated wind field and HRD wind field. HRD wind at Aug. 28 01:30 and 07:30 are used to interpolate the wind field at 04:30 (slide 7) and HRD wind at Aug. 28 04:30 and 10:30 are used to interpolate the wind field at 07:30 (slide 9).