Spatiotemporal Variations of Precipitation over Iran Using the High-Resolution and Nearly Four Decades Satellite-Based PERSIANN-CDR Dataset

被引:27
作者
Mosaffa, Hamidreza [1 ]
Sadeghi, Mojtaba [2 ]
Hayatbini, Negin [2 ]
Gorooh, Vesta Afzali [2 ]
Asanjan, Ata Akbari [2 ,3 ]
Phu Nguyen [2 ]
Sorooshian, Soroosh [2 ,4 ]
机构
[1] Shiraz Univ, Water Engn Dept, Shiraz 7196484334, Iran
[2] Univ Calif Irvine, Ctr Hydrometeorol & Remote Sensing CHRS, Henry Samueli Sch Engn, Dept Civil & Environm Engn, Irvine, CA 92697 USA
[3] Univ Space Res Assoc, Mountain View, CA 94043 USA
[4] Univ Calif Irvine, Dept Earth Syst Sci, 3200 Croul Hall, Irvine, CA 92697 USA
关键词
trend analysis; precipitation; satellite precipitation product; PERSIANN-CDR; Iran; CHANGE-POINT; TRENDS; PATTERNS; TEMPERATURE;
D O I
10.3390/rs12101584
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Spatiotemporal precipitation trend analysis provides valuable information for water management decision-making. Satellite-based precipitation products with high spatial and temporal resolution and long records, as opposed to temporally and spatially sparse rain gauge networks, are a suitable alternative to analyze precipitation trends over Iran. This study analyzes the trends in annual, seasonal, and monthly precipitation along with the contribution of each season and month in the annual precipitation over Iran for the 1983-2018 period. For the analyses, the Mann-Kendall test is applied to the Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks-Climate Data Record (PERSIANN-CDR) estimates. The results of annual, seasonal, and monthly precipitation trends indicate that the significant decreases in the monthly precipitation trends in February over the western (March over the western and central-eastern) regions of Iran cause significant effects on winter (spring) and total annual precipitation. Moreover, the increases in the amounts of precipitation during November in the south and south-east regions lead to a remarkable increase in the amount of precipitation during the fall season. The analysis of the contribution of each season and month to annual precipitation in wet and dry years shows that dry years have critical impacts on decreasing monthly precipitation over a particular region. For instance, a remarkable decrease in precipitation amounts is detectable during dry years over the eastern, northeastern, and southwestern regions of Iran during March, April, and December, respectively. The results of this study show that PERSIANN-CDR is a valuable source of information in low-density gauge network areas, capturing spatiotemporal variation of precipitation.
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页数:14
相关论文
共 59 条
  • [11] Climate change and changes in global precipitation patterns: What do we know?
    Dore, MHI
    [J]. ENVIRONMENT INTERNATIONAL, 2005, 31 (08) : 1167 - 1181
  • [12] Evaluation of precipitation datasets against local observations in southwestern Iran
    Fallah, Ali
    Rakhshandehroo, Gholam Reza
    Berg, Peter
    Sungmin, O.
    Orth, Rene
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2020, 40 (09) : 4102 - 4116
  • [13] Fulton RA, 1998, WEATHER FORECAST, V13, P377, DOI 10.1175/1520-0434(1998)013<0377:TWRA>2.0.CO
  • [14] 2
  • [15] Greve P, 2014, NAT GEOSCI, V7, P716, DOI [10.1038/ngeo2247, 10.1038/NGEO2247]
  • [16] Long-term spatio-temporal precipitation variations in China with precipitation surface interpolated by ANUSPLIN
    Guo, Binbin
    Zhang, Jing
    Meng, Xianyong
    Xu, Tingbao
    Song, Yongyu
    [J]. SCIENTIFIC REPORTS, 2020, 10 (01)
  • [17] Evaluation of PERSIANN-CDR for Meteorological Drought Monitoring over China
    Guo, Hao
    Bao, Anming
    Liu, Tie
    Chen, Sheng
    Ndayisaba, Felix
    [J]. REMOTE SENSING, 2016, 8 (05)
  • [18] Spatio-temporal evaluation of global gridded precipitation datasets across Iran
    Hosseini-Moghari, Seyed-Mohammad
    Araghinejad, Shahab
    Ebrahimi, Kumars
    [J]. HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES, 2018, 63 (11): : 1669 - 1688
  • [19] Hsu KL, 1997, J APPL METEOROL, V36, P1176, DOI 10.1175/1520-0450(1997)036<1176:PEFRSI>2.0.CO
  • [20] 2