Table of Contents


This conceptual model describes katabatic winds on the southeastern coast of Greenland, where they are called Piteraqs. These may be in some cases even hurricane-force (up to speed of 80 m/s) winds that rush down from the high glacier down to the coast trough valleys. The same kind of winds occurs also on the coasts of Antarctica.

This module describes Piteraqsoccurring near Tasiilaq's synoptic station:

Near Tasiilaq the ocean is mostly open throughout the year, whereas in middle and northern Greenland and in Antarctica the sea ice reaches the coast for the greatest part of the year. This leads to a phenomenom called Polynia, which is described in the chapter Meteorological Physical Background.

I. Cloud Structure In Satellite Images

Learn about how to recognise and detect Piteraq in satellite images.

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II. Meteorological Physical Background

Find out more about the meteorlogical and physical background of Piteraq.

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III. Key Parameters

Learn which key parameters to use for Piteraq.

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IV. Typical Appearance In Vertical Cross Sections

Find out the typical appearance of Piteraq in vertical cross section

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V. Weather Events

Explore the weather events associated with Piteraq

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VI. References

Let these comprehensive documents in the references assist you in finding more about Piteraq

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