'Specific humidity' diaporamas de présentation

Detection of Equatorial Waves in Data

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Modelling of transient vegetation and soil related processes

Modelling of transient vegetation and soil related processes. Patrick Samuelsson Swedish Meteorological and Hydrological Institute patrick.samuelsson@smhi.se. The Rossby Centre Regional Climate Model Land Surface Scheme (LSS) (Samuelsson and Gollvik)

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LESSON 3 THERMODINAMICS OF THE ATMOSPHERE

Environmental. Physics. LESSON 3 THERMODINAMICS OF THE ATMOSPHERE. Equation of state for an ideal gas. Gasses mixture Work and heat. The first law. Changes of phase Air parcel. Adiabatic processes. Water steam: Moist air. Saturation Moist air processes. Diagrams Vertical stability.

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Chapter 7 Water and Atmospheric Moisture

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Two key terms with which to begin: Specific humidity; Relative humidity.

Two key terms with which to begin: Specific humidity; Relative humidity. A. B. C.

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Near Surface

Near Surface. Wind/wave and surface roughness Air temperature Specific Humidity Pressure. Wind from passive remote sensing. Cloud motion winds and similars Wind at the sea surface from passive MW radiometry Sunglint. Data coverage (received).

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CHAPTER

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Chapter 7 Water and Atmospheric Moisture

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Graduate Course: Advanced Remote Sensing Data Analysis and Application

Graduate Course: Advanced Remote Sensing Data Analysis and Application A COMPARISON OF LATENT HEAT FLUXES OVER GLOBAL OCEANS FOR FOUR FLUX PRODUCTS Shu-Hsien Chou Department of Atmospheric Sciences, National Taiwan University shchou@atmos1.as.ntu.edu.tw. OBJECTIVES:

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Moisture Flux and Specific Humidity overlaid with Wind vectors (850mb)

Moisture Flux and Specific Humidity overlaid with Wind vectors (850mb). Moisture Flux Scale. Specific Humidity Scale. June 86. Moisture Flux & Winds . Specific Humidity & Winds. July 86. Moisture Flux & Winds . Specific Humidity & Winds. August 86. Moisture Flux & Winds .

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CWB M idterm Review 2011

CWB M idterm Review 2011. Forecast Applications Branch NOAA ESRL/GSD. New STMAS surface analysis software. A new version of STMAS surface analysis system is installed in CWB in May, 2011; It is multivariate, flow-, terrain, land-water dependent;

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P RINCIPLES of STABLE ISOTOPE METEOROLOGY

P RINCIPLES of STABLE ISOTOPE METEOROLOGY. ABSTRACT The heavy isotopes of water (HDO and H 2 18 O) act as tracers of atmospheric processes and motions. Three field experiments (Puerto Escondido, Mexico, KWAJEX, and CAMEX 4) show that

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Storm-scale data assimilation and ensemble forecasting for Warn-on-Forecast

Storm-scale data assimilation and ensemble forecasting for Warn-on-Forecast. 5 th Warn-on-Forecast Workshop Dusty Wheatley 1 , Kent Knopfmeier 2 , and David Dowell 3

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The mesoscale convection life cycle: building block or prototype for larger-scale tropical waves?

The mesoscale convection life cycle: building block or prototype for larger-scale tropical waves? . Brian Mapes @ U. of Miami Stefan Tulich, Jialin Lin @ NOAA ESRL/PSD (formerly CDC) Paquita Zuidema @ U. of Miami paper in press at Dynamics of Atmospheres and Oceans contact mapes@miami.edu.

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By: David S. Myers and Duane E. Waliser Presented by: Emily M. Riley 24 April 2007

Three-Dimensional Water Vapor and Cloud Variations Associated with the MJO during Northern Hemisphere Winter. By: David S. Myers and Duane E. Waliser Presented by: Emily M. Riley 24 April 2007. Outline. Motivation Data and Methodology Digression to examine weighting function Results

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Atmospheric Water

Atmospheric Water. Goals for today Review Exercise 1 Define measures of water vapor in air Define vapor pressure and its relation with temperature Water vapor in an atmospheric column Computation of precipitable water Patterns of water vapor and precipitable water in space and time

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Matthew A. Janiga and Chris D. Thorncroft University at Albany 3 rd AMMA Conference 7/24/2009

The impact of African easterly waves on the environment and characteristics of convection over West Africa. Matthew A. Janiga and Chris D. Thorncroft University at Albany 3 rd AMMA Conference 7/24/2009. Objectives.

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Large-scale atmospheric circulation characteristics and their relations to local daily precipitation extremes in Hesse

Anahita Amiri Department of Geography Justus Liebig University Giessen. Large-scale atmospheric circulation characteristics and their relations to local daily precipitation extremes in Hesse , central Germany. Objective. Challenges

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Water in the atmosphere

Water in the atmosphere. Water in the atmosphere exists in all 3 forms: solid, liquid, and vapor. Ice can change to water and then to vapor if heat is added to it. Ice can also change directly to vapor in a process known as sublimation if it is below freezing and the air is very dry .

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