Supported by
Parent Dataset
ARTIST, measurements in cold-air advection over ice
Data center: Norwegian Meteorological Institute / Arctic Data Centre,https://adc.met.no/ARIST,
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)Metadata Information
Access constraint: OpenUse constraint:
Investigator
Name: Jörg HartmannOrganisation: AWI Alfred Wegener Institute for Polar and Marine ResearchEmail: christof.luepkes@awi.deMetadata Author
Temporal extent
Start date: 1998-03-26T14:00:00ZEnd date: 1998-03-27T15:00:00Z
Child dataset(s)
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during one flight of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. Delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. A detailed description is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007)License :
Access: Open-
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during one flight of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. Delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. A detailed description is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open -
ARIST
Institutions: Norwegian Meteorological Institute / Arctic Data Centre, AWI Alfred Wegener Institute for Polar and Marine Research, Norwegian Meteorological Institute / Arctic Data CentreShow more...
Abstract:
Data from aircraft observations during two flights of the aircraft campaign ARTIST (Arctic Radiation and Turbulence Interaction Study) caried out by AWI 1998. The first set of delivered files contain data from on-ice flow over the Fram Strait (26 March 1998) including profiles of radiation fluxes in stratus clouds over a region with closed pack ice. The second set of delivered files contain data from a day with clod-air advection over the Barents Sea covered with sea ice. The cold-air advection causes slight unstable stratification over sea ice. A detailed description of both data sets is given in the Damocles Deliverable Report D2.3-01 by Lüpkes and Hartmann (2007). The case with cold-air advectiob is described also in Vihma et al. (2005, BLM, 117(2), 275-300)License :
Access: Open