20-Year Arctic Winter Seasonal Surface Temperature Trend
Here the 20-year seasonal surface temperature trend for the winter is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees (See color bar below).
Here the 20-year seasonal surface temperature trend for the winter is shown over the Arctic region. This animation shows the warming and cooling regions in steps from the regions of least change to the areas of greatest change. Blue hues indicate cooling regions; red hues depict warming. Light regions indicate less change while darker regions indicate more. The temperature scale used ranges from -0.4 to +0.4 degrees Celsius in increments of .02 degrees (See color bar below).
A high resolution image of the 20-Year Winter Seasonal Surface Temperature Trend
The associated color bar used
Credits
Please give credit for this item to:
NASA/Goddard Space Flight Center
Scientific Visualization Studio, Larry Stock, Robert Gersten
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Visualizer
- Cindy Starr (Global Science and Technology, Inc.)
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Scientist
- Josefino Comiso (NASA/GSFC)
Release date
This page was originally published on Thursday, October 23, 2003.
This page was last updated on Wednesday, May 3, 2023 at 1:56 PM EDT.
Series
This page can be found in the following series:Related papers
A rapidly declining perennial sea ice cover in the Arctic, Geophysical Research Letters, Vol. 29, No. 20, October 2002.
A rapidly declining perennial sea ice cover in the Arctic, Geophysical Research Letters, Vol. 29, No. 20, October 2002.
Datasets used
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Arctic Seasonal Temperature Trends [NOAA-7, 9, 11, 14, 16: AVHRR]
ID: 441
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.