کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5753632 1620488 2017 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Distribution and trends of the cold-point tropopause over China from 1979 to 2014 based on radiosonde dataset
ترجمه فارسی عنوان
توزیع و روند تروپوپوز سرد نقطه چین در سالهای 1979 تا 2014 براساس مجموعه داده های رادیووزند
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علم هواشناسی
چکیده انگلیسی


- The significant cooling rate of -0.70K/decade for the temperature of tropopause is reported over China during 1979-2014
- The height of tropopause over China is rising with the rate of 273 m/decade during 1979-2014.
- The latitudinal distribution and variations of height and temperature of tropopause are reported over China
- The nonuniform latitudinal and longitudinal distribution of trends of height (temperature) of tropopause are first presented
- Reconfirm the expansion of the tropics: the difference of tropopause temperature among latitudes is enlarging year by year

The variation trends of the cold-point tropopause (CPT) are presented using radiosonde observations from 77 stations over China during 1979-2014. The latitude regions over China from 18°N to 53°N are divided into 7 latitude zones with every 5° intervals, and the spatial areas of 18°N-53°N, 75°E-135°E are divided into 27 lattices with 5° × 10° grids. The annual-mean values of height-of-CPT (H-CPT) and temperature-of-CPT (T-CPT) are then calculated by all the available samples within each latitude and longitude bin. By using the least squares regression method, it is found that the H-CPT increases with the rate of 273 m/decade, and overall the significant cooling rate of − 0.70 K/decade for the T-CPT over the whole of China. Then, the trends and latitude distribution of H-CPT and T-CPT for each latitude zone are analyzed. The difference of H-CPT among latitude distribution characteristic is reducing year by year, and the difference of T-CPT is enlarging. The H-CPT displays a rising trend between 28°N-53°N latitude region with the positive change rates, and it has decline trend between 18°N-28°N latitude region with the negative change rates. The change rates of T-CPT are negative values for all latitude zones. At last, the nonuniform latitudinal and longitudinal distribution of long-term trends of H-CPT and T-CPT are first presented for each spatial cell.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Atmospheric Research - Volume 193, 1 September 2017, Pages 1-9
نویسندگان
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