The field experiment FRAMZY (in German: Framstraßen-Zyklonen; in English: Fram Strait Cyclones) 2002 took place in the Fram Strait region between Greenland and Spitsbergen and between 76-83¿N during the period 25 February to 25 March 2002. It was the second field experiment (following FRAMZY 1999) on cyclones in the Fram Strait and their impact on sea ice. The objectives of FRAMZY 2002 were to sample a data set in order to understand the processes of cyclone generation and sea ice forcing by the cyclones and to estimate the quality of atmospheric models in analysing and forecasting the cyclones and the quality of sea ice models in simulating the cyclone impacts on the sea ice. FRAMZY 2002 also aims to clarify the role of Fram Strait cyclone...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...
The field experiment BASIS 2001 took place in the Gulf of Bothnia of the Baltic Sea. The Finnish Res...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...
The Fram Strait Cyclone Experiment, FRAMZY 1999, took place in the Fram Strait and Greenland Sea reg...
In April 1999 the Fram Strait Cyclone Experiment, FRAMZY 1999, was performed in the Fram Strait and ...
The drift buoys experiment FRAMZY 2007 consisted of the deployment and tracking of an array of 29 dr...
The FRAMZY 2008 experiment aimed at the measurement of the sea ice drift in the Fram Strait and its ...
In March 2007 the field campaign FRAMZY took place in the region between Spitsbergen and Greenland. ...
The relation between sea ice drift and cyclone activity in the Fram Strait region was studied by bot...
The field experiment BASIS 1998 took place in the Gulf of Bothnia in the Baltic Sea in a boundary zo...
The field experiment ACSYS 1998 took place in the Greenland Sea west of Spitsbergen from 10 to 25 Ma...
During the international FRAMZY expedition in March 2002 in-situ observations of Fram Strait cyclone...
The field campaign LOFZY 2005 (LOFoten ZYklonen, engl.: Cyclones) was carried out in the frame of Co...
This study aims at the determination of a Fram Strait cyclone track and of the cyclone's impact on i...
The field campaign LOFZY 2005 (LOFoten ZYklonen, engl.: Cyclones) was carried out in the frame of Co...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...
The field experiment BASIS 2001 took place in the Gulf of Bothnia of the Baltic Sea. The Finnish Res...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...
The Fram Strait Cyclone Experiment, FRAMZY 1999, took place in the Fram Strait and Greenland Sea reg...
In April 1999 the Fram Strait Cyclone Experiment, FRAMZY 1999, was performed in the Fram Strait and ...
The drift buoys experiment FRAMZY 2007 consisted of the deployment and tracking of an array of 29 dr...
The FRAMZY 2008 experiment aimed at the measurement of the sea ice drift in the Fram Strait and its ...
In March 2007 the field campaign FRAMZY took place in the region between Spitsbergen and Greenland. ...
The relation between sea ice drift and cyclone activity in the Fram Strait region was studied by bot...
The field experiment BASIS 1998 took place in the Gulf of Bothnia in the Baltic Sea in a boundary zo...
The field experiment ACSYS 1998 took place in the Greenland Sea west of Spitsbergen from 10 to 25 Ma...
During the international FRAMZY expedition in March 2002 in-situ observations of Fram Strait cyclone...
The field campaign LOFZY 2005 (LOFoten ZYklonen, engl.: Cyclones) was carried out in the frame of Co...
This study aims at the determination of a Fram Strait cyclone track and of the cyclone's impact on i...
The field campaign LOFZY 2005 (LOFoten ZYklonen, engl.: Cyclones) was carried out in the frame of Co...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...
The field experiment BASIS 2001 took place in the Gulf of Bothnia of the Baltic Sea. The Finnish Res...
The Fram Strait is an important interface for the transfer of Arctic climate signals to the North At...