Polar night operation at Dome Concordia with Star Photometer and ICE-T

Aerosols play a crucial role in radiative transfer processes. For improving the results of modeling due to aerosol effects, a detailed determination of atmospheric aerosol is required. For the monitoring of aerosol optical depth in the Arctic, a Star photometer for polar night observation has been e...

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Bibliographic Details
Main Authors: Herber, Andreas, Gröschke, Andre, Vitale, V., Strassmeier, K.
Format: Conference Object
Language:unknown
Published: 2006
Subjects:
Antarctic
Arctic
Ny-Ålesund
The Antarctic
Antarc*
Antarctica
Ny Ålesund
polar night
Spitsbergen
Online Access:https://epic.awi.de/id/eprint/16646/
https://hdl.handle.net/10013/epic.26502
Description
Summary:Aerosols play a crucial role in radiative transfer processes. For improving the results of modeling due to aerosol effects, a detailed determination of atmospheric aerosol is required. For the monitoring of aerosol optical depth in the Arctic, a Star photometer for polar night observation has been established in Ny-Ålesund, Spitsbergen (79°N, 12°E) in 1996. AOD data from the Antarctic plateau are presently very sparse. Year-round aerosol measurements will close this gap and allow a detailed study of the inter-annual and seasonal variations of over the high interior plateau. It is planned to install a Star photometer in Antarctica at Dome Concordia (75°S, 123°E, 3230 m a.s.l) in 2009.

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