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A data set of in situ measurement of summer Arctic sea ice physical properties
With the global warming, the summer Arctic sea ice has experienced a series of changes. For example, the sea ice extent and thickness are reduced. Temperature, salinity and... -
Gaofen satellite partial data
Gaofen (GF) is a series of Chinese civilian remote sensing satellites for the state-sponsored program China High-definition Earth Observation System (CHEOS). The series data... -
GlobSnow Snow Extent (SE)
The GlobSnow SE processing system applies optical measurements in the visual-to-thermal part of the electromagnetic spectrum acquired by the ERS-2 sensor ATSR-2 and the Envisat... -
Ice Mass Balance Buyo data deployed in Arctic on 10.08.2018
Two sets of Ice Mass Balance buyo were deployed in Arctic during the CHINARE9. One works for 9 months and the other works for 14 months. Temperature profiles of... -
A dataset of glaciers in the Tanggula Mountains in 1991 and 2015
The Tanggula Mountains are located in the central part of the Tibetan Plateau (31°15′–34°45′N, 90°23′–95°52′E), are bordered by the Zulkkora Mountains to the west and by the... -
GlobSnow Snow Water Equivalent （SWE）
The GlobSnow SWE record, based on methodology by Pulliainen (Pulliainen 2006, Takala et al.2011) utilizes a data-assimilation based approach combining space-borne passive... -
A dataset of spatial distribution of degree-day factors for glaciers in High ...
The degree-day model, a widely used approach for ice and snow melt computation, rests upon a relationship between snow or ice melt and air temperature that is usually expressed... -
Phenological metrics dataset, land cover types map for the Tibetan Plateau an...
With abundant types and large coverage of alpine vegetation, the Tibetan Plateau has been a hot region for researches on the spatial distribution and phenological changes of... -
MODIS-based Daily Lake Ice Extent and Coverage Dataset for Tibetan Plateau
The Tibetan Plateau houses numerous lakes, the phenology and duration of lake ice in this region are sensitive to regional and global climate change, and as such are used as key... -
A dataset of glacier mass balance of Hailuogou catchment in Mount Gongga, sou...
Glacier mass balance is among the clearest natural indicators of ongoing climate change and is important for the assessment of water resources and sea-level rise. However, few... -
A dataset of glacier elevation change in Muztag Ata and Kongur Tagh from 1971...
While climate-driven glacier change significantly impacts regional water resources, particularly the hydrological cycle, glacier elevation change is a key indicator of climate... -
The Canadian Ice Thickness Program
he Canadian Ice Thickness Program has two data collections that users can access anytime online: Ice Thickness Program Collection, 1947 to 2002 [XLS;4.1 MB] | Metadata Ice... -
Dataset of MODIS-based Daily River Ice Fraction for the Arctic
Daily River Ice Fraction for the Arctic. -
Arctic sea ice melt pond fraction derived from MODIS
Melt pond fraction (MPF) on sea ice is an important factor for ice-albedo feedback throughout the Arctic Ocean. Based on The Moderate Resolution Imaging Spectroradiometer... -
Dataset of the May 2015 Karayaylak Glacier surge in eastern Pamir
Karayaylak Glacier (38°35′6″N–38°44′48″N, 75°7′47″E–75°22′29″E) is located in the northern slope of Jiubie Peak of Kongur Mountains, eastern Pamir, China. Its surge in May 2015... -
A dataset of glacier elevation changes in the Kangri Karpo Mountains during 1...
Due to the influence of the Indian monsoon, the Kangri Karpo Mountains, located in southeast Tibet, is the most humid and maritime glacier-concentrated region on the Tibetan... -
Data of sea ice drift in the 5th, 6th 7th and 8th CHINARE Arctic cruise
Sea ice position data collected by GPS buoys deployed in the 5th, 6th 7th and 8th CHINARE Arctic cruis. Data of sea ice drift collected by the buoys deployed in the 5th... -
Dataset of MODIS-based Daily Lake Ice Extent and Coverage for the Arctic
MODIS-based Daily Lake Ice Extent and Coverage for the Arctic
