'Land ocean' presentation slideshows

ACE Science Traceability Matrix: Oceans Science Team Mtg. March 10-12, 2009

ACE Science Traceability Matrix: Oceans Science Team Mtg. March 10-12, 2009. Chuck McClain NASA/GSFC. Recent Ocean Team Activities. ACE Ocean working group (weekly telecons) Bio-optical and aerosol model sensitivity to system and algorithm noise

396 views • 32 slides

The Tropics: Climatology and Large-Scale Circulations

The Tropics: Climatology and Large-Scale Circulations. Outline. Climatology Radiation Land / Ocean Temperature Winds Moisture Clouds and Precipitation Large-Scale Circulations Hadley Cell Walker Circulation. Sun. Earth. The Tropics: Climatology.

332 views • 23 slides

The Tropics: Climatology and Large-Scale Circulations

The Tropics: Climatology and Large-Scale Circulations. Outline. Climatology Radiation Land / Ocean Temperature Winds Moisture Clouds and Precipitation Large-Scale Circulations Hadley Cell Walker Circulation. Sun. Earth. The Tropics: Climatology.

348 views • 23 slides

ACE

ACE. Aerosol, Cloud, & Ocean Ecosystem Mission. A cross-disciplinary mission focused on climate forcings of the Earth system. Mission Chief Scientist David Starr, NASA Goddard Space Flight Center Ocean Lead: Charles McClain, NASA Goddard Space Flight Center

433 views • 20 slides

ACE

ACE. Aerosol, Cloud, & Ocean Ecosystem Mission. A cross-disciplinary mission focused on climate forcings of the Earth system. Mission Chief Scientist David Starr, NASA Goddard Space Flight Center Ocean Lead: Charles McClain, NASA Goddard Space Flight Center

318 views • 20 slides

All disasters

All disasters .

151 views • 7 slides

What causes a volcano to erupt?

What causes a volcano to erupt?. A volcano erupts when magma escapes from inside the earth. As the magma is escaping from a confined space, a lot of energy is released with it, as happens with any other explosion. The effects of volcanoes.

309 views • 6 slides

Representativeness CDAS v 1.1 Implementation

Representativeness CDAS v 1.1 Implementation. Model-data mismatch due to boundary-layer/stable-layer height errors and spatial flux heterogeneities Weighting in assimilation will be set using a parameterization based on land/ocean, day/night, z, and monthly NEE and FF

153 views • 3 slides

168 views • 1 slides