Deutscher Wetterdienst Welcome to Session 5, part 2 "Diagnosis of precipitation types from radar (practise)"

Slides:



Advertisements
Similar presentations
What creates different climates in Canada and what impact does climate have on human activity? The Climates of Canada.
Advertisements

Britains CLIMATE – a description Cool summers 13 / 17*C Mild winters4 / 7 *C Wet 600 – 2000 mms.
Weather Forecasting: Part 2
Why Do Climates Vary?.
Sequence for a cyclonic storm over western Europe Comparison with weather radar maps The radar images were provided by the INM, Spain, Dr Miguel A. Martinez.
Earth Systems and Patterns: SC.5.E.7.3
Synoptic Charts Weather Discussion 2009 Sarah Kew.
Viewing and Depicting the Atmosphere MODIS 03 FEB UTC
The Weather Observing and recording Powerpoint Presentation © Pitsford Hall weather station Northamptonshire Grammar School Abridged version without video.
Satellites and Radar – A primer ATMO 203. Satellites Two main types of satellite orbits – Geostationary Earth Orbiting Satellite is 35,786 km (22,236.
Chapter 5: Cloud Development and Precipitation Atmospheric Stability Atmospheric Stability Determining stability Determining stability Cloud development.
Ch. 16: Weather (#1-2).
How do we measure and forecast the weather?. Radar images can detect areas of rainfall and how heavy it is. RAINFALL.
What creates different climates in Canada and what impact does climate have on human activity? The Climates of Canada.
Climate. What Is Climate? Weather changes from day to day. However, the weather in any area tends to follow a pattern throughout the year. When you describe.
4-4.3 Compare daily and seasonal changes in weather conditions (including wind speed and direction, precipitation, and temperature) and patterns.
Facts and Questions Science and Weather By: De’Anna Jones, Bruce Aguon, Alex Spang and Jared Ruoff.
Forecasting Weather Maps Present a weather map to the class and explain how it forecasts the weather.
Do Now for Monday, Nov. 12 th. Look at this graph carefully. Calculate the 50% relative humidity at 30 degrees C.
2-1. A. Weather – condition of the bottom layer of the earth’s atmosphere in one place over a short period of time B. The weather in one place might be.
Chapter 2 Section 3 Winds.
Atmospheric Circulation. 1. Global Convection Currents Equator = warm  rising air Poles = cold  sinking air.
Using Doppler Radar to “Nowcast” Winter Storms...A Review MSC Winter Severe Weather Workshop Boulder February 2002.
Water Cycle and Weather. Georgia Performance Standards S4E3 Students will differentiate between the states of water and how they relate to the water cycle.
1.Weather – the condition of the earth’s atmosphere 2.Relative humidity – a measure of the amount of water vapor in the air compared with the amount.
Formation of the Extratropical Cyclone (Cyclogenesis)
Climatic Zones p P. 75 fig. 5.1.
Drizzle, Shallow Events Martin Hagen with the help from Elena Saltikoff, Paul Joe and others Deutsches Zentrum für Luft- und Raumfahrt (DLR) Oberpfaffenhofen,
Energy of the Atmosphere Sun – 98% of the energy in Earth’s atmosphere comes from the sun in the form of electromagnetic waves. Radiation – is the direct.
Blended Course on the Principles of Satellite Meteorology 21 st April – 15 th July 2009 Classroom June 2009 Final Presentation – Convection – 09May2009.
Chapter 2, Section 3. What is wind? The horizontal movement of air from an area of HIGH pressure to an area of LOW pressure.
Chapter 7: Climate Weather. Precipitation  Precipitation occurs when a cold air mass meets a warm air mass.  The cold air, being more dense, forces.
Weather & Climate. 1-Weather c onsists of: Atmosphere Temperature Humidity Precipitation rain, sleet, hail, and snow. Wind Cloud Cover.
SYNOPTIC OBSERVATIONS DECODING & PLOTTING. ENCODING WEATHER INFORMATION In order for people to send information around the world using the WMO discussed.
Earth Science Chapter 9.
Weather Patterns.
Climate Factors that affect our Climate. Weather The day-to-day characteristics of temperature, rain, cloud cover and wind Why is it important to know/inquire.
Read. Answer the following in your notebook:  What type of pressure systems produce hurricanes, tornadoes, and winter weather storms?  What things do.
Unit 3 Lesson 3 How Do We Measure Weather?
Weather Revision National 4/5. What is the difference between weather and climate? Weather is the day to day changes in the atmosphere. temperature precipitation.
What’s the Difference?. Climate or Weather?  Weather is the daily conditions of the atmosphere.  Weather changes day to day.  Weather = one day  Example:
A cloud is a visible aggregate of tiny water droplets and/or ice crystals suspended in the atmosphere They can exist in a variety of shapes and sizes.
Next Week: QUIZ 1 One question from each of week: –5 lectures (Weather Observation, Data Analysis, Ideal Gas Law, Energy Transfer, Satellite and Radar)
Chapter 5 Lesson 3 Global Patterns Pgs. 164 – 169 Benchmark: SC.6.E.7.3.
Types of Precipitation Precipitation comes in two forms Precipitation comes in two forms Liquid – rain, drizzle Liquid – rain, drizzle Solid - freezing.
Forecasting Winter Precipitation
Response of active and passive microwave sensors to precipitation at mid- and high altitudes Ralf Bennartz University of Wisconsin Atmospheric and Oceanic.
Climate is affected by Earth's Features
What causes the wind to blow?
Types of Precipitation Precipitation comes in three forms Precipitation comes in three forms Liquid – rain, drizzle Liquid – rain, drizzle Freezing – freezing.
Energy in Earth’s Atmosphere  Where does heat in the Atmosphere come from?  The sun.  In what form does this energy travel to Earth?  Electromagnetic.
Air Pressure & Wind Patterns. What is air pressure?  Air pressure is the force of molecules pushing on an area.  Air pressure pushes in all direction.
Chapter 7 Weather The condition of the atmosphere at a certain time and place. is affected by the amount of water in the air. Water in liquid, solid, and.
Weather & Climate.
How are they similar, how are they different?
Weather and meteorology npor. Eva Slovák Kubalová
Raleigh, North Carolina
Air Pressure Chapter 2, Section 1.
How do we measure Weather?
Happy Wednesday! Come in Quietly
Weather Symbols.
Weather and Climate.
Fronts By 2/O John Jaromahum.
Chapter 3 Weather and Climate.
Factors that Affect Climate
Winds.
What creates different climates in Canada and what impact does climate have on human activity? The Climates of Canada.
Water Cycle and Weather
Presentation transcript:

Deutscher Wetterdienst Welcome to Session 5, part 2 "Diagnosis of precipitation types from radar (practise)"

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Outline Diagnosis of precipitation type: Practical rules Technical limitations (base: DWD Radar Network) Examples Sections of radar reflectivities in accordance to model temps / sections? Bright band in relation to observations and AMDAR Doppler wind:  Cold air near surface, warmer above Additional remarks Questions and answers

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Radar beam's width and height distance Radar not applicable for diagnosing preciptiation types near the surface!

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), General Z-R–relation (DWD) Fixed values (independend in the season!) a = 256 and b= 1,42! In the meanwhile new radar products at DWD oimproved Z/R-relation oadjusted to measurements (RADOLAN)

Deutscher Wetterdienst Thresholds for precipitation types and intensities (DWD-products) dBZ mm/h(general Z/R-relation)Precipitation type and intensity 1 – 60,02negligible precipitation, drizzle, light snow ,06 - 0,4 light rain, snow (partly moderate) ,4 - 1,9light to moderate rain, moderate to heavy snow ,9 - 8,1moderate rain / shower, Winter: Thunderstorms, heavy snow ,1 - 35,0Summer: Heavy rain, shower, thunderstorm, Winter: heavy rain (seldom) and sleet , ,0Summer: Hazardous rain, heavy shower, thunderstorm, Winter: Sleet, graupel > 56 > 150,0Summer: Heavy thunderstorm (hail) Winter: Heavy sleet

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), General rules (Winter, middle latitudes) Snow of same intensity as rain: about 7 dBZ less Snow almost not possible : above 37 dBZ Rain seldom: above 37 dBZ  sleet? Rain not possible: above 46 dBZ  sleet  graupel Be careful: Attenuation possible (e.g., due to sleet) Low stratus Negative dBZ-values: only snow grains possible Positive dBZ-values, below 7 dBZ: (freezing) drizzle possible

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), , 14 UTC, Heavy snow (75) International composite (2x2 km): Violet, in that case hint to heavy snow, one green pixel ( ≥ 37 dBZ) DWD - Composite (1x1 km): partly even 37 to 40 dBZ Red elipse: Area of Bad Vilbel (our flat), Visibility about 100 m and 10 cm snow within 30 minutes!

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), , 00 UTC, Sleet – Bright band: Model temp correct Kassel Bavarian Forrest model-analysis: wet bulb temperature +1°C:1345 m  sleet (near snow line)

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), , 01 UTC: Clearly sleet 43 – 47 dBZ: Sleet (1000 m) Frankfurt (100 m): moderate rain (63) Automatic cell evaluation: Marker of significant summer convection ?!

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Bright band – snow line - significant weather – precipitation amount ( , 07 UTC) Precipitation amount derived from standard Z/R-relation: above 5 mm/h (in accordance to high reflectivities, below) (measurements less than 1 mm/h) Questions for you: 1.Please consider the lower image. Where do you expect sleet? Mark by using 2.In which height do you expect the transition from snow to rain? Please use again about 100 m about 1000 m about 2000 m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Answers Up to 41 dBZ (in 1 km height): Sleet AMDAR Frankfurt: T = 1°C (similar to wet bulb temperature during preciptiation) in 800 m ( ≈ 1 km)

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Indirect technique: Doppler, synops (800 and 2 m) Rhein-Main-Area, ) surface m: Wind from north to east above: Wind with west component  near surface cold, above warmer , 04 UTC Wind direction: 1000 m west component, near surface north,  thin layer of cold air , 07 UTC Kleiner Feldberg: 805 m , 07 UTC 10 UTC: 2m-wind now with south component 2km 12 km 1 km 805 m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Coincidence of mild and cold air over Germany to

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Situation ( , 06 UTC) COSMO-EU-6h-forecast: ps, T850, Sig weather, wind 10m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Situation ( , 18 UTC) COSMO-EU-6h-forecast: ps, T850, Sig weather, wind 10m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Situation ( , 18 UTC) COSMO-EU-6h-forecast: ps, T850, Sig weather, wind 10m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Situation ( , 12 UTC) COSMO-EU-analysis: ps, T850, Sig weather, wind 10m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Situation ( , 12 UTC) COSMO-EU-12h-forecast: ps, T850, Sig weather, wind 10m

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Precipitation type: Radar in context with other data sources , 19 UTC COSMO-DE-1h-forecast: Warmer air above colder air near surface Lower levels E-wind component Higher levels: westerly wind Snow Radar: Sleet, freezing rain, heavy snow (violet pixel) ? In contect of model section: be aware of freezing rain and as long as easter wind component freezing rain possible! West wind, however around 0°C, fluid precipitation according to radar Further to the west: Not critical, moderate rain and mild air 3° 2° 0° freezing rain? -2° height [hPa]

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Precipitation type: Radar in context with other data sources , 19 UTC COSMO-DE-1h-forecast: Warmer air above colder air near surface Lower levels E-wind component Higher levels: westerly wind Snow Radar: Sleet, freezing rain, heavy snow? In contect of model section: be aware of freezing rain and as long as eastern wind component freezing rain possible! Orange and red pixels: Sleet West wind, however around 0°C, fluid precipitation according to radar Further to the west: Not critical, moderate rain and mild air 3° 2° 0° freezing rain? -2° height [hPa ]

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), COSMO-DE-1h-forecast: T2m, sections (T, wind) / radar section / radar composite + significant weather/ ( , 11 UTC) > 60 dBZ 1 km above sea level! 1,5°C ≈ wet bulb temperature  sleet

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), COSMO-DE-analysis: T2m, sections (T, wind) / radar section / radar composite + significant weather/ ( , 18 UTC) 55 dBZ, in the meanwhile 1.8 km above sea level! 1,5°C ≈ wet bulb temperature  slee

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Question: Where do you expect the snow line? Please mark , 20 UTC

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Answer T ≈ 1.5°C

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Additional remarks Preciptiation types can be derived only indirectly from radar with polarimetric radar possible no information near the surface General synoptic situation should be taken into account General precipitation intensity  interpretation of radar images surface temperatures, wind and observations should be considered, too model data for the forecaster's sensibilisation useful Is freezing rain likely? Pixels of higher dBZ embedded in areas of lower dBZ  danger to freezing rain, other However, clutter in radar should be taken into account Is freezing rain not likely? Pixels of higher dBZ embedded in areas of lower dBZ  sleet or "normal" rain Again, clutter in radar should be taken into account

Deutscher Wetterdienst EUMeTrain-snow-week: Session 5 b), Thank you! Questions?