Thaw depth measurements from the Circumpolar Active Layer Monitoring (CALM) project for site 'Lorino' (R41), Chukotka, Russia from 2010-2018 ...

• Main Author: Streletskiy, Dmitry
• Format: Dataset
• Language: English
• Published: Arctic Data Center 2019
• Subjects: EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > ACTIVE LAYER; IN SITU/LABORATORY INSTRUMENTS > PROBES > TEMPERATURE PROBES; IN SITU/LABORATORY INSTRUMENTS > PROBES > SNOW MEASURING ROD; IN SITU/LABORATORY INSTRUMENTS > PROBES > SOIL TEMPERATURE PROBE; IN SITU/LABORATORY INSTRUMENTS > PROBES > SOIL DEPTH PROBE; IN SITU/LABORATORY INSTRUMENTS > RECORDERS/LOGGERS > TEMPERATURE LOGGERS; IN SITU/LABORATORY INSTRUMENTS > TEMPERATURE/HUMIDITY SENSORS > THERMISTORS > THERMISTORS; IN SITU/LABORATORY INSTRUMENTS > PROBES > SOIL MOISTURE PROBE; IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES; IN SITU/LABORATORY INSTRUMENTS > TEMPERATURE/HUMIDITY SENSORS > TEMPERATURE SENSORS; POINT; 1 METER TO 30 METERS; 30 METERS TO 100 METERS; 100 METERS TO 250 METERS; 250 METERS TO 500 METERS; 500 METERS TO 1 KILOMETER; 1 KILOMETER; MONTHLY TO ANNUAL; FIELD SURVEY; TRANSECT; GRID; MULTIPLE; GRIDS AND VECTORS; environment; Antarctic; Arctic; Lorino; Active layer monitoring; Active layer thickness; Antarc*; Chukotka; Climate change; permafrost; Subarctic
• Online Access: https://dx.doi.org/10.18739/a2xs5jh0q; https://arcticdata.io/catalog/view/doi:10.18739/A2XS5JH0Q

The primary goal of the Circumpolar Active Layer Monitoring (CALM) program is to observe the response of the active layer and near-surface permafrost to climate change over long (multi-decadal) time scales. The CALM observational network, established in the 1990s, observes the long-term response of the active layer and near-surface permafrost to changes and variations in climate at more than 200 sites in both hemispheres. CALM currently has participants from 15 countries. Majority of sites measure active-layer thickness on grids ranging from 1 hecatre to 1 square kilometer, and observe soil temperatures. Most sites in the CALM network are located in Arctic and Subarctic lowlands. Southern Hemisphere component (CALM-South) is being organized and currently includes sites in Antarctic and South America. The broader impacts of this project are derived from the hypothesis that widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the ...