Aerosols and Warming Change with Time - Version 1

  • Released Monday, August 13, 2001
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As the aerosol content and solar heating change with time, the atmosphere and the Earth's surface experience different warming and cooling. This animation displays a time series of the INDOEX region with 8-day averages showing aerosol and solar reflectance (albedo) data from the Terra satellite From these, we see how these inputs generate warming of the atmosphere (Atmospheric Forcing - red regions) and cooling of the surface (Surface Forcing - dark regions). Areas of missing data (due to clouds, etc.) are either black or transparent.

Video slate reads, 'Aerosols over INDOEX; Cooling the ground but warming the atmosphere; Version 1'.

Video slate reads, 'Aerosols over INDOEX; Cooling the ground but warming the atmosphere; Version 1'.



Credits

Please give credit for this item to:
NASA/Goddard Space Flight Center Scientific Visualization Studio

Release date

This page was originally published on Monday, August 13, 2001.
This page was last updated on Wednesday, May 3, 2023 at 1:57 PM EDT.


Missions

This page is related to the following missions:

Series

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Datasets used

  • [Terra: CERES]

    ID: 114
    Sensor: CERES Dates used: 2001/01/01-2001/03/21

    The CERES instrument aboard many Earth-orbiting satellites records the flow of reflected Solar radiation and reprocessed longwave radiation in the Earth's radiation budget.

    See all pages that use this dataset
  • [Terra: MODIS]

    ID: 116
    Sensor: MODIS Dates used: 2001/01/01-2001/03/21

Note: While we identify the data sets used on this page, we do not store any further details, nor the data sets themselves on our site.