Spatial-Temporal Distribution of Tropospheric Specific Humidity in the Arid Region of Northwest China

Based on the atmospheric temperature and dew point temperature difference series of mandatory levels in the arid region of northwest China, we calculated the specific humidity of stations at 200, 300, 400, 500, 700, and 850 hPa and analyzed the spatial and temporal distribution. The specific humidity of radiosonde is compared with two sets of reanalysis data (ERA-interim from European Centre for Medium Range Weather Forecasts and Modern Era Retrospective Analysis for Research and Applications: MERRA-2). The annual specific humidity and summer specific humidity show a positive trend in the vertical atmospheric levels during the period 1958-2018. Taking the middle of the 1980s and 2002 as boundaries, the selected levels show the trend of declining-gentle rising-fluctuation rising. The maximum specific humidity is observed at the level of 850-700 hPa during the warm months of the year, and the most vertical expansion in specific humidity is in July. In terms of spatial distribution, the specific humidity is greatly influenced by the topography and underlying surface at lower levels. The characteristics of spatial distribution of the trend are well described by the two sets of reanalysis data in the middle and upper levels, but there are some deficiencies in depicting the trend in the lower levels.

Automated summary

The study on the atmospheric temperature and dew point temperature differences in the arid region of northwest China revealed a positive trend in specific humidity in the vertical atmospheric levels over time. The specific humidity is greatly influenced by topography and underlying surface, with spatial distribution characteristics well described by reanalysis data in the middle and upper levels.