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Showing 1 through 7 of 7
Cryology Data at Riscos Rink, James Ross Island, Permafrost Monitoring Station [CDA_AR_CRIOLOGY_RISCOS_RINK_JRI]
Since 1995, the "Riscos Rink" Permafrost Monitoring Automatic Recorder Station has been recording: Air temperature Soil temperature Basement temperature on the active area of permafrost ...
Cryology Data from Automatic Recording Stations on James Ross Island, Antarctica [CDA_AR_CRIOLOGY_DATA]
The data includes air, soil, and basement temperatures from various automatic recording stations in Antarctica.
Cryology Data from Lachman Automatic Recording Climatological Station [CDA_AR_CRIOLOGY_LACHMAN]
Since 1992, Lachman Climatological Automatic Recorder Station has been recording: Air temperature; Humidity; Wind direction; Wind intensity; Solar Radiation; and Atmospheric pressure.
Cryology Data from Lachman Costa, James Ross Island, Permafrost Monitoing Station [CDA_AR_CRIOLOGY_LACHMAN_COSTA]
Since 1995, the "Lachman Costa", JRI. Permafrost Monitoring Station, positioned at 8 m height, has been gathering the following data: Air temperature; Soil temperature; and Basement ...
Cryology Data from Lachman Hornfels, James Ross Island, Permafrost Monitoring Station [CDA_AR_CRIOLOGY_LACHMAN_HORNFEL]
Since 2000, air, soil and basement temperatures have been recorded at specified intervals with soil and basement temperatures measured to 8 m in depth.
Cryology Data from Riscos Tumbledown, James Ross Island, Permafrost Monioring Station [CDA_AR_CRIO_RISCOS_TUMBLEDOWN]
Since 2001, the Riscos Tumbledown Permafrost Monitoring Station on James Ross Island has been measuring:: - Air temperature; - Soil temperature; and - Basement temperature to 2m in depth.
Data from the "MARAMBIO VOR" Permafrost Monitoring Automatic Recorder Station [CDA_AR_CRIOLOGY_MARAMBIO_VOR]
Since 1992, "MARAMBIO VOR" Permafrost Monitoring Automatic Recorder Station has been recording: Air temperature; Soil temperature; and Basement temperature down to 10 meters in depth.
Showing 1 through 7 of 7
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Responsible NASA Official:
Dr. Stephen Wharton
Last updated: May 2016