Grid-to-grid Model mixing ratio’s (RWMR[T>0]/SNMR) vs. MRMS ptype (rain/snow/none) Evaluation regarding how well each model explicit mixing ratios (>0.

Slides:



Advertisements
Similar presentations
Precipitation.
Advertisements

Case 2 15 March Case 3 2 – 3 April 2003.
 Know how to measure weather.  Know the tools we use it to measure weather.
Paul Fajman NOAA/NWS/MDL September 7,  NDFD ugly string  NDFD Forecasts and encoding  Observations  Assumptions  Output, Scores and Display.
N1 N2 N3 N4 N5 N6 N7 N8 N9 N10 N11 N12 N13 N14 N15 S1 S2 S3 S4 S5 S6 Figure 1: This map shows the four analyzed basins of the Ande Mountains of South America.
19 June summary So far quite incomplete. One hypothesis is that a windshift line approaches the ‘dryline’ from the west (the dry side) around 20:20 UTC,
Extreme Weather Tornado.
1.3 Weather and Climate. Weather and Climate What is the difference between the two?
1 04/03/02 01:30 utc IR. 2 04/03/02 02:00 utc IR.
1. White fluffy clouds with little or no precipitation 2. A cloud at ground level 3. Tall clouds with a flat base that bring thunderstorms 4. High wispy.
The March 01/02 Non-Winter Weather Event: Part 1 Michael W. Cammarata Anthony W. Petrolito.
Before you decide to do outdoor activities, it is important that you know what kind of weather it will be. If you look out and the sky is sunny without.
The 2014 Flash Flood and Intense Rainfall Experiment Faye E. Barthold 1,2, Thomas E. Workoff 1,3, Wallace A. Hogsett 1*, J.J. Gourley 4, and David R. Novak.
Geoterms.
National 5 Weather Factors affecting Rainfall[Date] Today I will: - Understand the four different factors which influence the rainfall.
Hot and Cold The Weather What’s the weather like in the north ?
The IOP6 (24 September 2012) heavy precipitation event over Southern France: observational and model analysis Lagouvardos, K. (1), Kotroni, V. (1), Bousquet.
Gracious and Compassionate. The Lord is gracious and compassionate Slow to anger, and rich in love The lord is gracious and compassionate Slow to anger,
Weather Tools. Scientists who study weather are called Meteorologists. A meteorologist uses tools to measure the weather. Read on to find out more about.
Speed and Acceration. distance Total distance an object travels from a starting point to ending point.
Quadratic Formula You can use this formula to find the solutions(roots) to a quadratic equation. This formula can be broken up into 2 parts: b 2 – 4ac.
MMET Team Michelle Harrold Tracy Hertneky Jamie Wolff Demonstrating the utility of the Mesoscale Model Evaluation Testbed (MMET)
Precipitation. What is precipitation? Precipitation is… …any form of water that falls from the sky.
Calculating Relative Humidity. Directions: Write the fraction then find the percentage. 1. There are 8 units of water in the air. At its current temperature,
Forecasting Winter Precipitation
Air Masses and Fronts. OBJECTIVE: IDENTIFY THE MAJOR TYPES OF AIR MASSES THAT EFFECT WEATHER IN NORTH AMERICA.
Topcon PG-A1 antenna TPSPG_A1+GP
DRAFT – Page 1 – January 14, 2016 Development of a Convective Scale Ensemble Kalman Filter at Environment Canada Luc Fillion 1, Kao-Shen Chung 1, Monique.
Warm up  Answer the following questions on the 5 themes of Geography:  Describe absolute and relative location.  Describe some positive and negative.
Idealized Tropical Cyclone Structure. Tropical Cyclone Extension of the Warm Core middle –level vortex to the surface. Inducement of Ekman pumping Non-linear.
Mrs. Tweedie April 2006 Vocabulary The Water Cycle.
Air Pressure and Fronts. Air Pressure Air has weight, and is in constant motion and is pulled towards Earth’s center by gravity. Air pressure is greatest.
ABIOTIC FACTORS in the Environment Pages KQ LEFT, NOTES RIGHT- CORNELL NOTE FORM.
1)Consideration of fractional cloud coverage Ferrier microphysics scheme is designed for use in high- resolution mesoscale model and do not consider partial.
Control Run Precipitation Comparison John D. McMillen.
West African Monsoon Experiment using RegCM2 + - Ernest A. Afiesimama - Ernest A. Afiesimama presenting …. presenting ….
4-8 Adding and Subtracting with Like Denominators Course 1 Warm Up Warm Up Lesson Presentation Lesson Presentation Problem of the Day Problem of the Day.
Regional-scale OSSEs used to explore the impact of infrared brightness temperature observations Jason Otkin UW-Madison/CIMSS 06 February 2013.
Characteristics of precipitating convection in the UM at Δx≈200m-2km
Climate Change Highlands, NC
TC Structure Theta_e Structure Grid 3: Vertical motion surfaces 15:30 UTC 26 August, m/s – red -1 m/s -blue +0.5 m/s – red -0.5 m/s -blue.
The Evaluation of Precipitation Information from Satellites and Models
How did the Cold War start?
Weather Tools.
Relevant publications
Raleigh, North Carolina
TAIWIN model verification task
Review Write an explicit formula for the following sequences.
Hadia and Mia The Meteorologists
10/6/11 BR: ______ is like Madison Ave. ____ is like State St
Measuring Distances and Directions
Errors in Satellite-based Precipitation Estimates Over Land
C/C Compare and contrast the political and economic characteristics of West and East African states from
Adding and Subtracting with Like Denominators 4-8
Statistical Inference for the Mean Confidence Interval
בטיחות בתעשייה בהיבט חברות הביטוח
BFB Thursdee, October 27th.
Key question / Learning outcomes
CAPS Real-time Storm-Scale EnKF Data Assimilation and Forecasts for the NOAA Hazardous Weather Testbed Spring Forecasting Experiments: Towards the Goal.
Longitude and Latitude
خطوات البحث العلمي.
Abiotic and Biotic Factors
Aim: How do we locate positions on Earth?
Adding and Subtracting with Like Denominators 4-8
Archived Data and Blank US Maps
NOAA Blended Total Precipitable Water
H64:02 Clear River East & West Hills Sept 8/99 (mvc-019f)
5.6 Sum of Geometric Series (1/4)
How fast objects travel
Question 1. Question 1 What is 10 x 40? A 40 B 400 C 4000 D 4.0.
Presentation transcript:

Grid-to-grid Model mixing ratio’s (RWMR[T>0]/SNMR) vs. MRMS ptype (rain/snow/none) Evaluation regarding how well each model explicit mixing ratios (>0 – could be very small) compared to the precipitation type information in the MRMS dataset (e.g., how well do the models discriminate precipitation type of rain or snow?) Broken down by 00 and 12 UTC initializations CONUS, CONUS-East, CONUS-West

PODy/PODn SNMR

FAR SNMR

GSS/Fbias SNMR

PODy/PODn RWMR>0

FAR RWMR>0

GSS/Fbias RWMR>0

Grid-to-point Model mixing ratio’s (RWMR[T>0]/RWMR[T≤0]/SNMR) vs. MPING and METAR MPING: RWMR[T>0]->MPING_RAIN RWMR[T≤0]->MPING_FRZR SNMR-> MPING_SNOW METAR: RA|DZ, but not FZ, --> METAR_RAIN SN, but not BLSN|DRSN, --> METAR_SNOW FZ, but not FZFG, --> METAR_FRZR PE|PL|GR|GS|SG, --> METAR_ICEP Any other string, but not UP, --> METAR_NONE Broken down by 00 and 12 UTC initializations CONUS, CONUS-East, CONUS-West

PODy/PODn MPING - SNMR

PODy/PODn METAR - SNMR

FAR MPING/METAR - SNMR

GSS/Fbias MPING - SNMR

GSS/Fbias METAR - SNMR

PODy/PODn MPING – RWMR ≤0

PODy/PODn METAR – RWMR ≤0

FAR MPING/METAR – RWMR ≤0

GSS/Fbias MPING – RWMR ≤0

GSS/Fbias METAR – RWMR ≤0

PODy/PODn MPING – RWMR >0

PODy/PODn METAR – RWMR >0

FAR MPING/METAR – RWMR >0

GSS/Fbias MPING – RWMR >0

GSS/Fbias METAR – RWMR >0