'Upper stratosphere' diaporamas de présentation

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I. Structure and Characteristics of the Atmosphere

I. Structure and Characteristics of the Atmosphere

I. Structure and Characteristics of the Atmosphere. A. Early atmosphere. Created from gases released from volcanoes – outgassing. Mostly water vapor, nitrogen, and carbon dioxide. Oxygen was not part of atmosphere until a long time later

By MikeCarlo
(82 views)

Decadal Variation of t he Holton-Tan Effect

Decadal Variation of t he Holton-Tan Effect

Decadal Variation of t he Holton-Tan Effect. Hua Lu , Thomas Bracegirdle, Tony Phillips , Andrew Bushell. DynVar /SNAP Workshops, 22-26 April, 2013, Reading, UK. U. T.

By addison
(123 views)

Thomason and Peter, 2006

Thomason and Peter, 2006

MIPAS observations of SO 2 and COS M. Höpfner 1 , N. Glatthor 1 , U. Grabowski 1 , S. Kellmann 1 , MKiefer 1 , A. Leyser 1 , A. Linden 1 , J. Orphal 1 , G. Stiller 1 , T. v. Clarmann 1 , C. Brühl 2 , J. Lelieveld 2 , C. Boone 3

By gaston
(108 views)

Radiative transfer in numerical models of the atmosphere

Radiative transfer in numerical models of the atmosphere

Radiative transfer in numerical models of the atmosphere. Robin Hogan Slides contain contributions from Jean-Jacques Morcrette, Alessio Bozzo,Tony Slingo and Piers Forster. Outline. Lectures 1 & 2 Global context From Maxwell to the two-stream equations Gaseous absorption and emission

By umeko
(175 views)

19-4 How Have We Depleted O 3 in the Stratosphere and What Can We Do?

19-4 How Have We Depleted O 3 in the Stratosphere and What Can We Do?

19-4 How Have We Depleted O 3 in the Stratosphere and What Can We Do? . Concept 19-4A Our widespread use of certain chemicals has reduced ozone levels in the stratosphere, which has allowed more harmful ultraviolet radiation to reach the earth’s surface.

By rhona
(133 views)

ATMOSPHERE

ATMOSPHERE

ATMOSPHERE . Grade 8 Science. What is the atmosphere??. Atmosphere is a thin layer of air or gases that surrounds earth and protects it from extreme temperature and harmful sun rays. Composition of Air.

By ethan
(155 views)

Lidar Measurements of Atmospheric State Parameters in the Mesosphere and Lower Thermosphere

Lidar Measurements of Atmospheric State Parameters in the Mesosphere and Lower Thermosphere

Lidar Measurements of Atmospheric State Parameters in the Mesosphere and Lower Thermosphere. Jonathan Friedman Arecibo Observatory Seminar 12 April 2007. Outline. Atmospheric Structure Lidar Technique Light Scattering From photons to state parameters Transmitter

By cayla
(162 views)

Concepts and infrastructures for GPM ground validation activity in Italy

Concepts and infrastructures for GPM ground validation activity in Italy

Concepts and infrastructures for GPM ground validation activity in Italy. Eugenio Gorgucci Istituto di Scienze dell’Atmosfera e del Clima Roma, Italy. Giorgio Roth CIMA Savona, Italy. Outline. Climatology of Italy Italian infrastructure for GPM GV

By masao
(136 views)

The Stratosphere: Point / Counterpoint

The Stratosphere: Point / Counterpoint

The Stratosphere: Point / Counterpoint. Solar Forcing. Coupler. Land. Atmosphere. Ocean. Sea Ice. C/N Cycle. Dyn. Veg. Ecosystem & BGC. Gas chem. Prognostic Aerosols. Upper Atm. Solar Cycle Studies: Model Input. Spectral composite courtesy of: Judith Lean (NRL) and

By tocho
(63 views)

Exploring the stratospheric/tropospheric response to solar forcing

Exploring the stratospheric/tropospheric response to solar forcing

Exploring the stratospheric/tropospheric response to solar forcing. D. Rind et al. 2010/03/30 Pei-Yu Chueh. Introduction. Higher values in the upper troposphere are reported, seen most clearly during June-August although present on the annual average.

By malana
(94 views)

Layers of the Atmosphere

Layers of the Atmosphere

Layers of the Atmosphere. Layers. The four main layers are called the troposphere, the stratosphere, the mesosphere, and the thermosphere The four main layers are classified according to temperature. The Troposphere. The lowest layer of the Earth’s atmosphere (where we live)

By garin
(311 views)

The ASSET Intercomparison project (ASSIC)

The ASSET Intercomparison project (ASSIC)

The ASSET Intercomparison project (ASSIC). Author: W.A. Lahoz Thanks to ASSET partners Data Assimilation Research Centre, University of Reading RG6 6BB, UK. You want to do chemical DA… You ask: What model should I use? What DA scheme should I use? What data should I assimilate?

By demont
(106 views)

A signal in the energy due to planetary wave reflection in the upper stratosphere

A signal in the energy due to planetary wave reflection in the upper stratosphere

A signal in the energy due to planetary wave reflection in the upper stratosphere. J. M. Castanheira (1), M. Liberato(2), C. DaCamara(3) and J. M. P. Silvestre(1) – Department of Physics, University of Aveiro, 3810-193 Aveiro, Portugal

By mollie-burks
(77 views)

Aura in a Historical Context

Aura in a Historical Context

(a). (b). (c). (d). Aura in a Historical Context. Long-term time-series of HCl and Cl y.

By ramona-harmon
(69 views)


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