Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Daxing site-large aperture scintillometer) (2008-2010)

The dataset contains large aperture scintillator flux observation data from January 1, 2008, solstice, December 31, 2010.The station is located in weishanzhuang, daxing district, Beijing.The latitude and longitude of the observation point are 116.4271E, 39.6213N and 20m above sea level. The acquisition frequency of the large aperture scintillation instrument is 1Hz, the effective height is 29.6m, the optical diameter length is 2480m, the longitude and latitude of the transmitting end is 116.4271E, 39.6213N, and the longitude and latitude of the receiving end is 116.4369E, 39.6422N.The data released by the large aperture scintillator is the average data of 30min after processing and quality control, in which the sensible heat flux is mainly obtained by combining with the data of automatic meteorological station and by iterative calculation based on the moning-obhoff similarity theory.(2) eliminate data with weak demodulation signal strength;(3) data of the time of precipitation and the hour before and after the precipitation are excluded;(4) data of weak turbulence under stable conditions were excluded (u* < 0.1m/s). Data released by the large aperture scintillator include: Date/Time Date/Time, air refractive index structure parameter Cn2 (m-2/3), sensible heat flux H_LAS (W/m2) Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Daxing site - eddy covariance system) (2008-2010)

The dataset contains vortex correlator observation data from January 1, 2008, solstice, December 31, 2010.The station is located in weishanzhuang, daxing district, Beijing.The latitude and longitude of the observation point are 116.4271E, 39.6213N and 20m above sea level. The acquisition frequency of the eddy correlates instrument is 10Hz, the frame height is 3m, the ultrasonic direction is 295 ° (due north direction is 0 °), and the distance between the ultrasonic anemometer and the CO2/H2O analyzer is 18cm.The published data is the 30-minute data obtained by the post-processing of the original collected 10Hz data with Edire software. The main steps of the processing include: outfield value elimination, delay time correction, coordinate rotation (plane fitting), frequency response correction, ultrasonic virtual temperature correction and density (WPL) correction.Quality assessment for each intercompared to at the same time, mainly is the atmospheric stability (Δ st) and turbulent characteristics of similarity (ITC) test.The 30min pass value output by Edire software was also screened :(1) the data when the instrument was wrong was removed;(2) data of 1h before and after precipitation were excluded;(3) the missing rate of 10Hz original data is more than 3% every 30min;(4) the observed data of weak turbulence at night were excluded (u* less than 0.1m/s).The average period of observation data was 30 minutes, 48 data a day, and the missing data was marked as -6999. The observation data released by vortex correlator include:Date/Time for the Date/Time, wind Wdir (°), Wnd horizontal wind speed (m/s), standard deviation Std_Uy lateral wind speed (m/s), ultrasonic virtual temperature Tv (℃), the water vapor density H2O (g/m3), carbon dioxide concentration CO2 (mg/m3), friction velocity Ustar) (m/s), the length of cloth hoff, sensible heat flux Hs (W/m2), latent heat flux LE (W/m2), carbon dioxide flux Fc (mg/(m2s)), the quality of the sensible heat flux identifier QA_Hs, the quality of the latent heat flux identifier QA_LE,Carbon dioxide flux mass identification QA_Fc.The quality of the sensible heat and latent heat, carbon dioxide flux identification is divided into nine grades (quality logo 1: (0 < Δ st < 15, 0 < ITC < 30);2: (16 < < 30, 0 < ITC Δ st < 30);3: (0 < Δ st < 30, 31 < ITC < 75);4: (31 < < 75, 0 < ITC Δ st < 30);5: (0 < Δ st < 75, 31 < ITC < 100);6 (76 < < 100, ITC Δ st < 100);7: (Δ st < 250, ITC < 250);8: (Δ st < 1000, ITC < 1000);The rest are 9).The meaning of data time, such as 0:30 represents the average between 0:00 and 0:30;The data is stored in *.xls format. Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Daxing site-automatic weather station) (2008-2010)

The data set contains observations from the automatic weather station as of 31 December 2010 as of 1 solstice January 2008.The station is located in weishanzhuang, daxing district, Beijing.The latitude and longitude of the observation point are 116.4271E, 39.6213N and 20m above sea level. The acquisition frequency of the automatic weather station is 10s, and the output of 10min is once.The observation factors include air temperature and relative humidity (10m), and the direction is due to the north.Wind speed (27m), wind direction (27m), heading due north;Air pressure (installed in waterproof box);Rainfall (30m);Four - component radiation (28m), the direction is due to the south;Infrared surface temperature (28m), the arm is facing south, the probe is facing vertically downward;The soil temperature and humidity probe was buried 2m south of the meteorological tower. The buried depth of the soil temperature probe was 2cm, 5cm, 10cm, 20cm, 40cm, 60cm, 80cm and 100cm. The buried depth of the soil water sensor was 2cm, 5cm, 10cm, 20cm, 40cm, 40cm, 60cm and 100cm.Two soil hot plates (2) were buried 2cm underground, one under the vegetation and the other between the trees.Processing and quality control of observation data :(1) ensure 144 data per day (every 10min). If data is missing, it will be marked by -6999;(2) eliminate the moments with duplicate records;(3) data that is obviously beyond the physical meaning or the range of the instrument is deleted;(4) the format of date and time is unified, and the date and time are in the same column.For example, the time is: June 10, 2010 at 10:30. Data released by the automatic weather station include:Date/Time, air temperature and humidity observation (Ta_10m, RH_10m) (℃, %), wind speed (Ws_27m) (m/s), wind direction (WD_27m) (°), pressure (Press) (hpa), precipitation (Rain) (mm), four-component radiation (DR, UR, DLR_Cor, ULR_Cor, Rn) (W/m2), surface radiation temperature (IRT_1, IRT_2) (℃),Soil heat flux (Gs_1, Gs_2) (W/m2), multi-layer soil moisture (Ms_2cm, Ms_5cm, Ms_10cm, Ms_20cm, Ms_40cm, Ms_60cm, Ms_100cm) (%) and multi-layer soil temperature (Ts_2cm, Ts_5cm, Ts_10cm, Ts_20cm, Ts_40cm, Ts_60cm, Ts_80cm, Ts_100cm) (℃). Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Haihe River Basin (Guantao site-large aperture scintillometer) (2008-2010)

The data set contains large aperture scintillator flux observation data from January 1, 2008, solstice, December 31, 2010.The site is located in hezhai village, guantao county, hebei province.The latitude and longitude of the observation point is 115.1274E, 36.5150N, and the altitude is 30m. The acquisition frequency of the large aperture scintillation instrument is 1Hz, the effective height is 15.6m, the optical diameter length is 2760m, the longitude and latitude of the transmitting end is 115.1284E, 36.5274N, and the longitude and latitude of the receiving end is 115.1249E, 36.5028n.The data released by the large aperture scintillator is the average data of 30min after processing and quality control, in which the sensible heat flux is mainly obtained by combining with the data of automatic meteorological station and by iterative calculation based on the moning-obhoff similarity theory.(2) eliminate data with weak demodulation signal strength;(3) data of the time of precipitation and the hour before and after the precipitation are excluded;(4) data of weak turbulence under stable conditions were excluded (u* < 0.05m/s). Data released by the large aperture scintillator include: Date/Time Date/Time, air refractive index structure parameter Cn2 (m-2/3), sensible heat flux H_LAS (W/m2). Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Guantao site-automatic weather station) (2008-2010)

The data set contains observations from the automatic weather station as of 31 December 2010 as of 1 solstice January 2008.The site is located in hezhai village, guantao county, hebei province.The latitude and longitude of the observation point is 115.1274E, 36.5150N, and the altitude is 30m. The acquisition frequency of the automatic weather station is 10s, and the output of 10min is once.The observation factors include air temperature and relative humidity (12.5m), and the direction is due north.Wind speed (12.7m), wind direction (12.7m), heading due north;Air pressure (installed in waterproof box);Rainfall (16m);Net radiation/four-component radiation (15.6m), facing due south;Infrared surface temperature (15.7m), the arm is facing south, the probe is facing vertically downward;The soil temperature and humidity probe was buried 2m south of the meteorological tower. The buried depth of the soil temperature probe was 0cm, 2cm, 5cm, 10cm, 20cm, 40cm, 60cm, 80cm and 100cm. The buried depth of the soil moisture sensor was 2cm, 5cm, 10cm, 10cm, 10cm, 10cm, 20cm, 60cm, 80cm and 100cm.Two soil hot plates (2) were buried 2cm underground, one under the vegetation and the other between the trees.Processing and quality control of observation data :(1) ensure 144 data per day (every 10min). If data is missing, it will be marked by -6999;(2) eliminate the moments with duplicate records;(3) data that is obviously beyond the physical meaning or the range of the instrument is deleted;(4) the format of date and time is unified, and the date and time are in the same column.For example, the time is: June 10, 2010 at 10:30. Data released by the automatic weather station include:Date/Time, air temperature and humidity observation (ta_12.5m, rh_12.5m) (℃, %), wind speed (ws_12.7m) (m/s), wind direction (wd_12.7m) (°), pressure (Press) (hpa), precipitation (Rain) (mm), four-component radiation (DR, UR, DLR_Cor, ULR_Cor, Rn) (W/m2), surface radiation temperature (IRT_1, IRT_2) (℃),Soil heat flux (Gs_1, Gs_2) (W/m2), multi-layer soil moisture (Ms_2cm, Ms_5cm, Ms_10cm, Ms_20cm, Ms_40cm, Ms_60cm, Ms_100cm) (%) and multi-layer soil temperature (Ts_0cm, Ts_2cm, Ts_5cm, Ts_10cm, Ts_20cm, Ts_40cm, Ts_60cm, Ts_80cm, Ts_100cm) (℃). Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Haihe River Basin (Miyun site-large aperture scitillometer) (2008-2010)

The data set contains large aperture scintillator observations from January 1, 2008, at solstice, December 29, 2010.The site is located in xinchengzi town, miyun county, Beijing, with orchards (plums and apple trees), corn/bare land, and towns.The latitude and longitude of the observation point is 117.3233E, 40.6308N, and the altitude is 350m. The acquisition frequency of the large aperture scintiometer is 1Hz, the effective height is 35.86m, the optical diameter length is 2420m, the longitude and latitude of the transmitting end is 117.3319E, 40.6446N, and the longitude and latitude of the receiving end is 117.3174E, 40.6254N.The data released by the large aperture scintillator is the average data of 30min after processing and quality control, in which the sensible heat flux is mainly obtained by combining with the data of automatic meteorological station and by iterative calculation based on the moning-obhoff similarity theory.(2) eliminate data with weak demodulation signal strength;(3) data of the time of precipitation and the hour before and after the precipitation are excluded;(4) data of weak turbulence under stable conditions were excluded (u* < 0.1m/s). Data released by the large aperture scintillator include: Date/Time Date/Time, air refractive index structure parameter Cn2 (m-2/3), sensible heat flux H_LAS (W/m2). Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-09

Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Miyun site-eddy covariance system) (2008-2010)

The data set contains vortex related flux observation data on January 1, 2008, solstice, December 29, 2010.The site is located in xinchengzi town, miyun county, Beijing, with orchards (plums and apple trees), corn/bare land, and towns.The latitude and longitude of the observation point is 117.3233E, 40.6308N, and the altitude is 350m. The acquisition frequency of the eddy correlativity instrument is 10Hz, the frame height is 26.66m, the ultrasonic direction is due to the north, and the distance between the ultrasonic anemometer and the CO2/H2O analyzer is 25cm.The published data is the 30-minute data obtained by the post-processing of the original collected 10Hz data with Edire software. The main steps of the processing include: outfield value elimination, delay time correction, coordinate rotation (plane fitting), frequency response correction, ultrasonic virtual temperature correction and density (WPL) correction.Quality assessment for each intercompared to at the same time, mainly is the atmospheric stability (Δ st) and turbulent characteristics of similarity (ITC) test.The 30min pass value output by Edire software was also screened :(1) the data when the instrument was wrong was removed;(2) data of 1h before and after precipitation were excluded;(3) the missing rate of 10Hz original data is more than 3% every 30min;(4) the observed data of weak turbulence at night were excluded (u* less than 0.1m/s).The average period of observation data was 30 minutes, 48 data a day, and the missing data was marked as -6999. The observation data released by vortex correlator include:Date/Time for the Date/Time, wind Wdir (°), Wnd horizontal wind speed (m/s), standard deviation Std_Uy lateral wind speed (m/s), ultrasonic virtual temperature Tv (℃), the water vapor density H2O (g/m3), carbon dioxide concentration CO2 (mg/m3), friction velocity Ustar) (m/s), the length of cloth hoff, sensible heat flux Hs (W/m2), latent heat flux LE (W/m2), carbon dioxide flux Fc (mg/(m2s)), the quality of the sensible heat flux identifier QA_Hs, the quality of the latent heat flux identifier QA_LE,Carbon dioxide flux mass identification QA_Fc.The quality of the sensible heat and latent heat, carbon dioxide flux identification is divided into nine grades (quality logo 1: (0 < Δ st < 15, 0 < ITC < 30);2: (16 < < 30, 0 < ITC Δ st < 30);3: (0 < Δ st < 30, 31 < ITC < 75);4: (31 < < 75, 0 < ITC Δ st < 30);5: (0 < Δ st < 75, 31 < ITC < 100);6 (76 < < 100, ITC Δ st < 100);7: (Δ st < 250, ITC < 250);8: (Δ st < 1000, ITC < 1000);The rest are 9).The meaning of data time, such as 0:30 represents the average between 0:00 and 0:30;The data is stored in *.xls format. Please refer to Jia et al.(2012) for information of observation test or site, and Liu et al.(2013) for data processing.

0 2020-03-08

Multi-scale surface flux and meteorological elements observation dataset in the Hai River Basin (Miyun site-automatic weather station) (2008-2010)

The data set contains observations from the automatic weather station as at 1 solstice, January 2008, on 29 December 2010.The site is located in xinchengzi town, miyun county, Beijing, with orchards (plums and apple trees), corn/bare land, and towns.The latitude and longitude of the observation point is 117.3233E, 40.6308N, and the altitude is 350m. The acquisition frequency of the automatic weather station is 10s, and the output of 10min is once.The observation factors include air temperature and relative humidity (30.56m, 10.66m), and the direction is due to the north.Wind speed (30.56m, 10.66m), wind direction (30.56m), heading due north;Air pressure (installed in waterproof box);Rainfall (31.46m);The four-component radiation (30.76m) is oriented due to the south.Infrared surface temperature (30.76m), the arm is facing south, the probe is facing vertically downward;The soil temperature and humidity probe was buried 2m south of the meteorological tower. The buried depth of the soil temperature probe was 0cm, 5cm, 10cm, 20cm, 40cm, 60cm, 80cm and 100cm. The buried depth of the soil water sensor was 2cm, 5cm, 10cm, 20cm, 40cm, 60cm and 100cm.Two hot plates (2) are buried 2cm underground, one in the ground where the sun can penetrate the fruit trees, and the other in the shadow of the fruit trees.Processing and quality control of observation data :(1) ensure 144 data per day (every 10min). If data is missing, it will be marked by -6999;(2) eliminate the moments with duplicate records;(3) data that is obviously beyond the physical meaning or the range of the instrument is deleted;(4) the format of date and time is unified, and the date and time are in the same column.For example, the time is: June 10, 2010 at 10:30. Data released by the automatic weather station include:Date/Time for the Date/Time, and the air temperature humidity observation (Ta_10. 66 m, RH_10. 66 m, Ta_30. 56 m, RH_30. 56 m) (℃, %), wind speed (Ws_10. 66 m, Ws_30. 56 m) (m/s), wind (WD) (°), pressure (Press) (hpa), precipitation (Rain) (mm), four component radiation (DR, UR, DLR, ULR, Rn) (W/m2), the surface radiation temperature (IRT_1, IRT_2) (℃),Soil heat flux (Gs_1, Gs_2) (W/m2), multi-layer soil moisture (Ms_2cm, Ms_5cm, Ms_10cm, Ms_20cm, Ms_40cm, Ms_60cm, Ms_100cm) (%) and multi-layer soil temperature (Ts_0cm, Ts_5cm, Ts_10cm, Ts_20cm, Ts_40cm, Ts_60cm, Ts_80cm, Ts_100cm) (℃). Please refer to Jia et al,(2012) for information of observation test or site, and Liu et al,(2013) for data processing.

0 2020-03-08

Spatial layout of characteristic agriculture in Qinghai Tibet Plateau

The data includes the county-level data of characteristic agriculture distribution in the Qinghai Tibet Plateau, which lays the foundation for the spatial distribution and development of characteristic agriculture in the Qinghai Tibet Plateau. The data are from the development plan of Tibet Plateau characteristic agricultural products base (2015-2020), Qinghai province's 13th five year plan, Sichuan Province's 13th five year plan for agricultural and rural economic development, Xinjiang Uygur Autonomous Region's 13th five year plan for targeted poverty alleviation of agricultural characteristic industries (2016-2020), Yunnan Province's overall plan for plateau characteristic agricultural modernization( 2016-2020), implementation opinions on fostering and strengthening characteristic agricultural industries in Gansu Province to boost poverty alleviation, China National Geographic Indication product network (http://www.cgi.gov.cn/home/default/), regional layout planning of characteristic agricultural products (2013-2020). The data is the distribution of county-level characteristic agriculture, realizing the spatialization of county-level characteristic agriculture. The data can be applied to the research on the spatial distribution of characteristic agriculture and the development of characteristic agriculture in the future.

0 2020-01-09