You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.
You must be logged in to perform this action.

QuikSCAT Antarctic Sea Ice (WMS)QuikSCAT Antarctic Sea Ice (WMS)

No Strings Attached
Author:
,
Subject:
Science and Technology
Institution Name:
NASA
Collection:
NASA GSFC Scientific Visualization Studio
Grade Level:
Secondary, Post-secondary
Abstract:

The sea ice around Antarctica grows dramatically from late February, when large parts of the coast are ice-free, to October, when the amount of sea ice effectively doubles the size of the continent. The SeaWinds Scatterometer instrument on the QuikSCAT satellite captures this dramatic ebb and flow and shows the sea ice as dynamic and always moving, even in areas that are ice-bound. This animation shows the sea ice around Antarctica from SeaWinds during 2004. SeaWinds can see individual icebergs if they are large enough, and a large iceberg can be seen for most of the year south of South America as it moves from the Antarctic Peninsula to the South Sandwich Islands. Also visible are the very convoluted and dynamic border between the sea ice and the open sea and holes in the sea ice created by the movement around fixed land features such as islands.

Course Type:
Learning Module
Languages:
English
Material Type:
Other
Media Format:
Graphics/Photos, Text/HTML, Video
Technical Requirements:
Real player
Conditions of Use:
Public Domain
Please give credit to NASA GSFC Scientific Visualization Studio

Comments:

Send link to this page

The e-mail address to send this link to.
A comment about this link.

Rate and Review

Evaluate Resource What is this?

Common Core Standards

Align this item
Not Yet Aligned

    Add new alignment tag:

    Share

    Tags

    Keywords, descriptive words, interested groups & more