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Entry ID: CN_NADC_2010-2013_Zhongshan_Station_To_Dome_A_Chinese_Antarctic_Zhongshan_Station_to_Dome_A_ION_CHROMATOGRAPHS_Nitrate_concentrations_in_snow
Publish Date: 2018-02-06
Author: Shi Guitao
Keywords: Dome A, Snow-Ice, nitrate, East Antarctica, Atmospheric Chemistry
Dataset: Files(1) Filesize(28.6 KB)
Summary: "Nitrate concentrations in in surface snow and snowpit on the traverse from coast (Zhongshan Station) to Dome A". Note that the citation of the data should be updated once the manuscript has been accepted. "This data set is that used in Shi et al., 2017 and should be cited as such:" "Shi G., Hastings M.G., Yu J., Ma T., Hu Z., An C., Li C., Ma H., Jiang S. and Li Y. (2017) Nitrate deposition and preservation in the snowpack along a traverse from coast to the ice sheet summit (Dome A) in East Antarctica. The Cryosphere Discuss. 2017, 1-27. doi:10.5194/tc-2017-227" In total, 20 snowpits, SP1-P20, and 120 surface snow samples were analyzed
Entry ID: CN_NADC_2009_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(100.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2009, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2008_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(19.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2008, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2016_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Author: Jin Shuang, Ma Hongmei, ,
Keywords: Austre Lovénbreen Glacier, Pedersenbreen Glacier, Arctic, huanghe Station, Glacier Mass Balance
Dataset: Files(1) Filesize(90.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2016, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2014_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(78.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2014, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2013_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(81.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2013, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2011_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(86.0 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2011, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2010_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(24.9 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2010, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2015_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(80.5 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.
Entry ID: CN_NADC_2012_Arctic_Chinese_Arctic_Yellow_River_Staion_Sensor_Description
Publish Date: 2017-07-24
Keywords: Arctic, huanghe Station, Austre Lovénbreen Glacier, Pedersenbreen Glacier, Glacier Mass Balance
Dataset: Files(1) Filesize(26.1 KB)
Summary: The 22 monitoring benchmarks are embedded in the A glacier and P glacier near the Chinese Arctic Yellow River station in 2012, which is used to carry out the observation of ice material balance.The equipment used is the snow ruler and the density scale.The ice material balance takes the direct measurement method, which is to set the fixed pole on the surface of the glacier, and observe the position of the glacier surface at the peak of the pole.The slope of the bar is measured by the Angle of the standard and the horizontal plane, and then the vertical distance between the peak of the benchmark and the surface of the glacier is calculated.Through this method, the net material balance of the entire glacier is obtained by the net material balance of the entire glacier.The measuring accuracy reached the centimeter level.