Forecasting Workshop 2009 Ryan Alliss, Andy Mair, Matt Hoffman.

Slides:



Advertisements
Similar presentations
Weather.
Advertisements

Accessing and Interpreting Web-based Weather Data Clinton Rockey National Weather Service Portland, Oregon.
Weather Dynamics in Earth’s Atmosphere. An atmosphere is a blanket of a gases surrounding a planet. Earth’s atmosphere has distinct layers defined by.
Mid-Latitude Cyclones: Vertical Structure
Chapter 4. Atmospheric Pressure and Wind
UPPER AIR DYNAMICS (continued) MSC 243 Lecture #8, 10/22/09.
#4095. How much colder than standard temperature is the actual temperature at 9,000 feet, as indicated in the excerpt from the Winds and Temperature Aloft.
Weather, Winds, and Fronts
Moist Processes ENVI1400: Lecture 7. ENVI 1400 : Meteorology and Forecasting2 Water in the Atmosphere Almost all the water in the atmosphere is contained.
Next Week: QUIZ One question from each of week: –9 normal lectures + global warming lecture –Over main topic of lecture and homework Multiple choice,
Natural Environments: The Atmosphere
Chapter 8 Coordinate Systems.
Chapter 7 Atmospheric Pressure and Wind
Topic VI “Meteorology”
Pressure and Winds. Aneroid Barometer Reading Pressure.
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
Supplemental Topic Weather Analysis and Forecasting.
Chapter 9 Meteorology. Section A, Weather Factors §Atmosphere l Comprised of: Oxygen - 21% Nitrogen - 78% Other gases - 1% l 99.9% of Atmosphere is within.
Weather Weather is the state or condition of the atmosphere at a particular location for a short period of time. Different weather is created by changes.
Weather Station Models Meteorologists use a system of assignment and coding to report a variety of weather conditions at a single location on a weather.
Weather Forecasting - II. Review The forecasting of weather by high-speed computers is known as numerical weather prediction. Mathematical models that.
Pressure, Wind and Weather Systems � WINDS are horizontal flows of air; winds blow from areas of high pressure to areas of low pressure (nature tries to.
SC.912.E.7.5 Predict future weather conditions based on present observations and conceptual models and recognize limitations and uncertainties of such.
General Circulation & Thermal Wind
GROUP # 5 UPDATED 02/20/07 Faye Barthold Michelle Benny Ting Sun.
Chapter 2 Section 3 Winds.
Upper Air Charts By Tom Collow November 8, Reading Upper Air Charts Temperature (°C) Dewpoint Depression (°C) Height Wind direction and speed (knots)
Meteorology 2 Review.
Formation of the Extratropical Cyclone (Cyclogenesis)
The Atmosphere: An Introduction to Meteorology, 12th
Objectives Review Vocabulary
Team 1 Meteorologists Hilary Minor & Matt Sanders.
Thickness and Thermal Wind /aos101/wk12.html /aos101/wk12.html.
Properties of the Atmosphere
METR March Review Hydrostatic balance Ideal gas law p = ρ R d T v, ρ = p / R d T v Take layer average virtual temperature, R and g as constants.
Humidity Under what conditions do you see the above?
What set the atmosphere in motion?
1 n Weather Maps – –We use weather maps to give us a pictorial view of the weather when dealing with large amounts of data. – –We typically report: » »Temperature.
Fronts Chapter 17 Section 1 Pages Chapter 17 Section 1 Pages
Lecture 4 (9/30) METR 1111 Station Plots and Fronts.
ATS/ESS 452: Synoptic Meteorology Friday 2/8/2013 Quiz & Assignment 2 Results Finish Thermal Wind MOS decoding (Assignment) New England weather.
Surface Condensation Water vapor condensing on large surfaces is called dew. Dew Point is the temperature that saturation occurs and condensation begins.
Forecasting Winter Precipitation
Where are they? Why is there no weather?. Meteorology The study of weather Good sites for weather info: weather.com
Understanding Weather Maps Signs and symbols. Low Pressure Low pressure means cloudy weather and precipitation are on the way Low pressure systems have.
Unit 4 Lesson 5 Notes Answer Key
Do Now: Air rises ___________ and ____________ Air rises ___________ and ____________ Air sinks ___________ and ____________ Air sinks ___________ and.
Weather. What is Weather????? Weather Animation Weather Definition Weather – state or condition of the variables of the atmosphere at a given time Weather.
To View Slide Show Click on “Slide Show” above –Click on “From Current Slide”
Composition of the Atmosphere Layers of the Atmosphere.
Recap……. Name the air masses…... Name the weather…..
Starter…Name these clouds… A B C DE F G H I. Answers… A. Cirrus B. Cirrocumulus C. Cirrostratus D. Altocumulus E. Altostratus F. Cumulonimbus G. Stratocumulus.
Key Concepts 1 Weather is the atmospheric conditions, along with short-term changes, of a certain place at a certain time. Variables used to describe weather.
Aim: What is relative humidity? Do Now: Answer the following in your notebooks; 1)What do you think of when you hear it is humid out? 2)Explain what type.
What’s the difference between Weather and Climate?
Air Pressure & Humidity. What is Air Pressure? The force exerted onto an object by the weight of air.
Fronts Front The Boundary between two different air masses.
AIR MASSES AND FRONTS By: Ms. Nail.
Dynamics in Earth’s Atmosphere
AOS 101 Cyclone Structure April 22/24 April 29/May 1.
Thickness and Thermal Wind
What direction do high and low pressure systems spin
Weather ©Mark Place,
Weather ©Mark Place,
Dynamics in Earth’s Atmosphere
Unit 4 Weather about Doppler Radar.
Robert Fovell Meteorology – Lecture 16 Robert Fovell
Air Masses and Fronts Earth Science Chapter 24.
Air Masses What are major air masses?
Presentation transcript:

Forecasting Workshop 2009 Ryan Alliss, Andy Mair, Matt Hoffman

WxChallenge Rules and Information All rules found at WxChallenge.com – Forecasts due at 0z, forecasting for 6z to 6z the following day Example for today’s forecast – Verification of forecasts by ASOS and Climatology information – Forecast Monday-Thursday – You can forecast for three days in advance if busy

Awards and Tournament Win a trophy if you finish first in your Category for a given period – Fresh/Soph-Cat 4, Junior/Senior- Cat 3, etc.. At the end of the year if you are in the top 64 nationally you will participate in a tournament to crown the top forecaster.

ISU WxChallenge Page Site made for ISU students regarding WxChallenge – ge/ ge/ Links can be altered for any asos site through input of station Results for ISU will be posted in results section All necessary information can be found here.

Submitting Forecasts Found at ISU WxChallenge page on left – “Enter Forecast” Or go directly to WxChallenge.com – Go to submit forecast tab Enter Username, Password, and School (ISU) Enter Forecast for Day 1, Hit Submit – If busy the following days you can forecast ahead for Day 2 and 3

Basic Meteorology Forecasting Red Book – Required for Mt111 and Mt311 – Contains all necessary info for forecasting Green Book – Optional We will sum up key concepts

UTC Time Greenwich Mean Time 0z is 7pm local time 12z is 7am local time When daylight savings time begins 0z will be 6pm and 12z will be 6am Forecasts for wxchallenge due at 0z, therefore you will have to send your forecasts in by 6pm when daylight savings time begins.

Pressure, units in millibars (mb) Pressure decreases with height – Surface around 1000mb – 30,000 ft around 500mb – Weight of the column of air above Pressure also varies horizontally – Surface lows and highs – Main contributor to wind, horizontal pressure gradients – Areas of Low pressure cause disturbed weather

Plotting at different levels Surface plots plot varying pressure Upper level plots use isobaric level and then plot varying heights – 500, 850, 700, 500 mb charts – Lower heights associated with lower pressure and thus more disturbed weather and vice versa for higher heights Temperature, humidity, wind speed, and direction also are plotted anywhere.

Surface METARS Plot basic information of the weather at a surface station

Clouds and Humidity Dewpoint – Measurement of amount of water vapor in the air – When dewpoint=temperature air is saturated Relative Humidity – Complicated equation, not used much outside of tv forecasts Clouds – Occur when a level is near saturation, at least RH>70%

Fronts Are defined by the line between air masses Formed off of areas of low pressure Converging winds cause upward motion, cloud cover, rain/snow Four main types of fronts – Cold Front – Warm Front – Occluded Front – Stationary Front

Satellite Imagery Visible – Reflection of light to satellite, what you would see if you were in space Infrared – Measures temperature of clouds – Clouds higher up are colder – Use at night Water Vapor – Measures water vapor in UPPER atmosphere – Used for seeing upper level circulations

Skew-ts Plot temperature, dewpoint, wind speed and direction with height Used to see where clouds are at – Dewpoint close to temp Severe Weather Forecasting applications – Instability, wind shear You will see these again

Low and High Pressure Low Pressure – Try to make equilibrium so more mass goes to low – Upward motion at surface yields disturbed weather – Winds circulate counter-clockwise and in High Pressure – Downward motion yields clear skies and calm winds – Winds circulate clockwise and out

Troughs and Ridges Waves exist in the atmosphere caused by pressure and temperature gradients Look at 500mb chart to find troughs and ridges East side of trough – Upward motion, location of surface low East side of ridge – Downward motion, location of surface high Trough=bad weather, Ridge=good weather

How to Forecast What are we forecasting for? – Max and Min Temperature, Max Sustained Wind Speed, and Liquid Precip Equivalent. Iowa Forecast Contest gives you more – Free Contest – Visibility, Ceiling, forecasting out past day 1… – Contact Jon Hobbs to join

Resources for Forecasting Models – Sager Model Animator- Images of Model Output – MOS (model output statistics) Human Guidance – NWS Point Forecast and Hourly Weather Graph Persistence Forecasting – Past observations that are similar to current situation All of these can be accessed at ISU WxChallenge Page

Models Use complex equations to “model” atmospheric behavior Outputted in the form of data that is converted to imagery Two main models used most often – GFS, Global Forecasting System Longer range model, poor resolution – NAM, North American Model Shorter range model, higher resolution

Maximum Temperature Things that affect Max Temp – Cloud Cover – Rain cooled air – Temp Advection Example- Winds blowing warmer air into area – Wind Speed – Adiabatic Motions Air flowing over mountain – More to come in later Meteorology Classes – Frontal Passage

Maximum Temperature cont. Start with persistence forecast then edit according to any of the effects that are now occurring – Example: Today’s High: 76, it was Clear with winds out of the south with high pressure dominating. Tomorrow’s most likely weather: Clouds moving in with winds shifting to the north, cold front sweeps through. – What should you expect the High to trend to?

I want numbers though! Once you know how the high will compare to tomorrow from today go to the models and NWS to compare. – MOS Max and Min Temps in Row “N/X”, 3 hr temps are in Row “TMP” – Point Forecast Provides Max and Min temps for NWS Over time you will be able to quantify in your head how much difference between days the High will be from changing conditions, without looking at the models and relying on them.

Maximum Temperature Strategy Go to 850 mb chart, find nearest station, take the temperature at 12z, add 13 degrees C to it and that is an estimation for the high tomorrow. Remember to convert to f – Example – Will not work if front passes I’m not a huge fan of this method.

Minimum Temperature Things that affect min temp – Cloud Cover – Wind Speed – Frontal Passage – Rain Cooled Air – Snow Cover – Temp Advections Exact same effects right?

Minimum Temperature Strat. Look at that dewpoint! – If it is clear and calm winds, good chance the temp will reach the dewpoint overnight – Sometimes forecasting the min temp involves forecasting the dewpoint as well What do you look at to forecast dewpoint? – MOS, Hourly Weather Graph, Trends Look at both ends of period, back door lows occur

Max Sustained Wind Speed What causes wind? – Pressure Gradient Force What lowers “ideal” wind speed? – Friction – Curvature in flow How to forecast – Look at forecast pressure gradients Surface MSLP contours – Use MOS, Hourly Weather Graph, and USL Model

MSLP Plot, Pressure Gradients!

Precipitation Forecasting Liquid Water Equivalent in inches. – Rain amount as is – For snow you use liquid water equivalent after it melts Around 1” water for 10” snow (1/10 ratio) – Heavier, wet snow yields more of a 1/8 ratio – Dry, fluffy snow yields more of a 1/12 ratio Forecasting exact amount – Mteor Classes will forecast by categories rather than exact amounts

Precip Cont. How to forecast – Find general area of forcing East side of Trough PVA- Positive Vorticity Advection Fronts/convergent regions – Model Output 24 hour qpf forecast MOS – Uses Categories » Cat 0=0”, Cat 1=Trace-.05”, Cat 2= ”, Cat 3=.25-.5”, Cat 4=.5-1.0”, Cat 5=>1”

Precip Cont. – Human Forecasts HPC QPF Hourly Weather Graph – All can be accessed from ISU WxChallenge Page – Models tend to overestimate Be weary of bullseyes or ribbons of precip – More points gained at smaller amounts You forecast 0”, and it verifies to.08” is more points gained than forecasting 1” and it verifies to 1.08” – Precip can be very tough or very easy

Forecasting Snowfall mb Thickness 540 line – If you are below 5400 m in thickness your layer is suitable for snowfall – Soundings Majority of layer must be below 32 degrees Human Forecasts – Look at what NWS has to say LIQUID WATER EQUIVALENT!

Forcing, Troughs, PVA

Same time, Precip, MSLP

24 hr Precip

Let’s Forecast! Go to the following page: – Come up with the four things we forecast for – Max Temp – Min Temp – Max Sustained Wind Speed – Precip Amount

How did we do? What actually happened in Boston? Important to look at verification to see if you did good and if not why – Look at 72 hr obs Was there cloud cover which you did not take into account or some other effect? This is the key to becoming a good, experienced forecaster

Questions?