'Low albedo' diaporamas de présentation

Thermal Infrared Remote Sensing Lecture 7

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I. Biogeochemical cycles

I. Biogeochemical cycles. The Carbon Cycle. A. The carbon cycle i. The global movement of carbon between organisms and the abiotic environment is known as the carbon cycle

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Dennis Baldocchi University of California, Berkeley NCEAS Workshop, Santa Barbara 2009

Land surface - boundary layer interactions . Dennis Baldocchi University of California, Berkeley NCEAS Workshop, Santa Barbara 2009. Case Study: Energetics of a Grassland and Oak Savanna Measurements and Model.

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Thermal Energy Transfer and the Sun

Thermal Energy Transfer and the Sun. Thermal Energy and Climate. Thermal Energy Transfer. BACKGROUND INFO: All things are made up of molecules When things get heated, they absorb heat energy With more energy, molecules are able to move faster

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The hazard of impacts from space

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Snow in Climate Models

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Super Greenhouse Effect Detection from Aqua instruments

Super Greenhouse Effect Detection from Aqua instruments. Dan Feldman Notes for DC Trip 10/16/05. Clear-sky greenhouse parameter. g increases linearly with SST for SST<298K g increases at a much faster rate for SST>298 K From Ravel and Ramanathan (1989) using ERBE data.

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SNR Basic Column Retrieval R. De Beek, M. Weber, R. Siddans (RAL), B. Latter (RAL)

SNR Basic Column Retrieval R. De Beek, M. Weber, R. Siddans (RAL), B. Latter (RAL) SNR output from RAL noise model program (PR1, Section 1.3). SNR calculation for 0.1875 sec GOME pixels (corresponding to integration of 10 successive LOS in CDI simulations) and 30 sec IT solar irradiance.

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Albedo

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