07 June 1998, 13:08 UTC, NOAA 14, Czech Republic

Slides:

Advertisements

Similar presentations

WHERE WE CAME FROM AND WHERE WE ARE HEADING PAN-Europe Annual meeting 4 September 2009 Sofia Bulgaria.

Advertisements

Dynamical processes at the storm top PAO K. WANG DEPARTMENT OF ATMOSPHERIC AND OCEANIC SCIENCES UNIVERSITY OF WISCONSIN-MADISON MADISON, WISCONSIN, USA.

Cloud Development and Forms

16 January 2008 Convective storm with warm plumes and cold-U shape near Maputo Martin Setvák MARTIN SETVÁK MARTIN SETVÁK

Petra Mikuš DHMZ, Croatia, EUMeTrain project 1.

HET Enclosure Temperature Readings Night of 5 September 2002 By: John Good Basement Ceiling Pier Wall High Mid Low Pier Top Pier Base Outer FloorInner.

ATMOSHERE The earth's atmosphere is a very thin layer wrapped around a very large planet. Two gases make up the bulk of the earth's atmosphere: nitrogen,

Satellite Rainfall Estimation Robert J. Kuligowski NOAA/NESDIS/STAR 3 October 2011 Workshop on Regional Flash Flood Guidance System—South America Santiago.

Chapter 27 - Clouds Use of Power Point design and animations with permission from Dr. Joby Hilliker ( West Chester University, West Chester, PA.

Lecture 1 Geraint Vaughan. Radiosondes Vaisala RS80 Vaisala RS92 Launching a radiosonde European radiosonde stations (launch 00 and 12 UTC) Data available.

Stability & Skew-T Diagrams

Lecture 10 Static Stability. General Concept An equilibrium state can be stable or unstable Stable equilibrium: A displacement induces a restoring force.

Thunderstorms ASTR /GEOL Physics of Thunderstorms Two fundamental ideas: Convection Latent heat of vaporization/condensation.

Possibility of stratospheric hydration by overshooting analyzed with space-borne sensors Suginori Iwasaki (National Defense Academy, Japan) T. Shibata.

Monsoon Meteorology ATS 553. Monsoon: A reversal of the wind direction at the surface, usually accompanied by the change in the precipitation regime,

RGB Airmass and Dust products NASA SPoRT CIRA. RGB Air Mass RED (6.2 – 7.3) –vertical moisture distribution GREEN ( ) – tropopause height based.

Air’s density changes two ways heat What happens to the air pressure on my head as the temperature increases?

Blended Course on the Principles of Satellite Meteorology 21 st April – 15 th July 2009 Classroom June 2009 Final Presentation – Convection – 09May2009.

Physics of the Atmosphere II

Temperature By: David Garcia P.5.

Air Stability Adiabatic Processes No heat is added / removed from the moving air parcel by the external environment because of fast movement of.

Cloud Formation. What are Clouds? Condensation of water vapor.

Purpose To deepen your knowledge of satellite images' interpretation  Preparation for the succeeding part about summer convection.

temperature Gases Layers Density Misc.

Chapter 15, Section 4 By Stephanie Lund September 27, 2005 T4.

Modeling GOES-R µm brightness temperature differences above cold thunderstorm tops Introduction As the time for the launch of GOES-R approaches,

Heat and Work.  Thermodynamics looks at how changes in energy, work and the flow of heat influence each other.

Cyclones and Anticyclones September 19, Name that cloud.

A Simple 2-Dimensional Chaotic Thunderstorm Model with Rain Gushes Stanley David Gedzelman Department of Earth and Atmospheric Sciences and NOAA CREST.

Violent Weather Chp 20.

Layers of Earth’s atmosphere. How was the atmosphere formed? Atmosphere has changed (evolved) over time. Gases are held near the surface by gravity. Earth’s.

1 Second Law of Thermodynamics Engines and Refrigerators.

Atmospheric Stability Terminology I Hydrostatic Equilibrium –Balance, in the vertical, between PGF and gravity –The general state of the atmosphere –Net.

Thermal Properties of Troposphere September 10, 2007.

Topic: Weather and The Atmosphere  Weather is the ______ or _______ of the ________ of the _________ at any given location for a __________  Weather.

Lab 9 – Due Nov 14 Chapter 13 10a,b,c Chapter 14 3a,b Chapter 15 1a,d 5a,b,c 6 8a,b,c 11a.

Experience in numerical forecast verification in the Hydrometeorological Centre of Russia N. P. Shakina, E. N. Skriptunova, A. R. Ivanova Zürich 2005 COSMO.

Laws of Thermodynamics. Zeroth Law of Thermodynamics “If two thermodynamic systems are each in thermal equilibrium with a third, then they are in thermal.

Storm Top Processes Related to the Cross ‐ Tropopause Transport Potential Applications of START08 Data Pao K. Wang Department of Atmospheric and Oceanic.

Satellite Survey of Tropical Deep Convection Particularly Stratospheric Penetrators William B. Rossow 12 June 2006.

The Convective Rainfall Rate in the NWCSAF

METEOSAT SECOND GENERATION (MSG)

METEOSAT SECOND GENERATION (MSG)

Robert Fovell Meteorology – Lecture 10 Robert Fovell

METEOSAT SECOND GENERATION (MSG)

Collaborative Effort for High Quality Training

Weather & Climate The Atmosphere.

Composition A mixture of Changes according to altitude and location.

Natural Sciences Grade 7

Lab 2: Vertical Structure of the Atmosphere

Objective Overshooting Top and Cold V Detection

Severe Weather and Storm Chasing

Layers of Earth’s atmosphere

Changes in the Free Atmosphere

Earth’s Atmosphere.

Layers of Earth’s atmosphere

Layers of Earth’s atmosphere

Above anvil plumes and jumping cirrus

Unit: Water and the Atmosphere Lesson 3: Layers of the Atmosphere

METEOSAT SECOND GENERATION (MSG)

6.1: Properties of the Atmosphere

METEOSAT SECOND GENERATION (MSG)

Session 4 Introduction User Engagement Activities

Jochen Kerkmann (EUMETSAT)

Layers of Earth’s atmosphere

MPEF DIVergence product Interpretation scheme

METEOSAT SECOND GENERATION (MSG)

Simultaneous observation of above-anvil ice plume and plume-shaped BTD anomaly atop a convective storm Mária Putsay, André Simon, Martin Setvák, Ildikó.

EART30351 Lecture 2.

Presentation transcript:

07 June 1998, 13:08 UTC, NOAA 14, Czech Republic If the top of a cell has penetrated into the tropopause or the lower stratosphere then the cloud top temperature in the middle of the dome will be warmer than the surrounding area, supposing that the cloud top is in thermal equilibrium with its environment. Cloud top at thermal equilibrium with its environment NIMH – EUMETSAT workshop, 25 – 29 September 2006 Sofia, Bulgaria Martin Setvák

07 June 1998, 13:08 UTC, NOAA 14, Czech Republic The overshooting top is much colder than the environment due to adiabatic cooling. Cloud top at thermal equilibrium with its environment, and with an overshooting top (penetrating “bubble”) NIMH – EUMETSAT workshop, 25 – 29 September 2006 Sofia, Bulgaria Martin Setvák

Main storm top features as seen by satellite (25 June 2006) NIMH – EUMETSAT workshop, 25 – 29 September 2006 Sofia, Bulgaria Martin Setvák