Stratospheric Temperature Anomalies

The stratosphere is the upper middle part of the atmosphere, and is the level of the Jet Stream winds. Colder temperatures in the stratosphere over the Arctic are associated with the positive phase of the Arctic Oscillation, and are indicative of stronger polar winds.

Keywords

OnLine resource: Open Science Catalog ( application/json )
Open Science Catalog

OnLine resource: Description ( text/html )
Description

OnLine resource: Variables ( application/json )
Variables

File identifier: stratospheric-temperature-anomalies XML

Hierarchy level: catalog catalog

Metadata standard name: ISO19115

Metadata standard version: 2003/Cor.1:2006

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