Bias Correction of Global High-Resolution Precipitation Climatologies Using Streamflow Observations from 9372 Catchments

被引:131
作者
Beck, Hylke E. [1 ]
Wood, Eric F. [1 ]
McVicar, Tim R. [2 ,3 ]
Zambrano-Bigiarini, Mauricio [4 ,5 ]
Alvarez-Garreton, Camila [5 ,6 ]
Baez-Villanueva, Oscar M. [7 ,8 ]
Sheffield, Justin [9 ]
Karger, Dirk N. [10 ]
机构
[1] Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08544 USA
[2] CSIRO Land & Water, Canberra, ACT, Australia
[3] Australian Res Council, Ctr Excellence Climate Extremes, Canberra, ACT, Australia
[4] Univ La Frontera, Dept Civil Engn, Temuco, Chile
[5] Ctr Climate & Resilience Res, Santiago, Chile
[6] Univ Austral Chile, Inst Conservat Biodivers & Terr, Valdivia, Chile
[7] Technol Arts Sci TH Koln, Inst Technol & Resources Management Trop & Subtro, Cologne, Germany
[8] TU Dortmund Univ, Fac Spatial Planning, Dortmund, Germany
[9] Univ Southampton, Sch Geog & Environm Sci, Southampton, Hants, England
[10] Swiss Fed Res Inst WSL, Birmensdorf, Switzerland
关键词
Precipitation; Rainfall; Snowfall; Data mining; Bias; Mountain meteorology; WATER-BALANCE; GRIDDED PRECIPITATION; OROGRAPHIC PRECIPITATION; RANDOM FORESTS; ANNUAL RUNOFF; CLIMATE; BASIN; SNOW; ACCURACY; GAUGE;
D O I
10.1175/JCLI-D-19-0332.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
070601 [气象学];
摘要
We introduce a set of global high-resolution (0.05 degrees) precipitation (P) climatologies corrected for bias using streamflow (Q) observations from 9372 stations worldwide. For each station, we inferred the "true" long-term P using a Budyko curve, which is an empirical equation relating long-term P, Q, and potential evaporation. We subsequently calculated long-term bias correction factors for three state-of-the-art P climatologies [the "WorldClim version 2" database (WorldClim V2); Climatologies at High Resolution for the Earth's Land Surface Areas, version 1.2 (CHELSA V1.2 ); and Climate Hazards Group Precipitation Climatology, version 1 (CHPclim V1)], after which we used random-forest regression to produce global gap-free bias correction maps for the P climatologies. Monthly climatological bias correction factors were calculated by disaggregating the long-term bias correction factors on the basis of gauge catch efficiencies. We found that all three climatologies systematically underestimate P over parts of all major mountain ranges globally, despite the explicit consideration of orography in the production of each climatology. In addition, all climatologies underestimate P at latitudes >60 degrees N, likely because of gauge undercatch. Exceptionally high long-term correction factors (>1.5) were obtained for all three P climatologies in Alaska, High Mountain Asia, and Chile-regions characterized by marked elevation gradients, sparse gauge networks, and significant snowfall. Using the bias-corrected WorldClim V2, we demonstrated that other widely used P datasets (GPCC V2015, GPCP V2.3, and MERRA-2) severely underestimate P over Chile, the Himalayas, and along the Pacific coast of North America. Mean P for the global land surface based on the bias-corrected WorldClim V2 is 862 mm yr(-1) (a 9.4% increase over the original WorldClim V2). The annual and monthly bias-corrected P climatologies have been released as the Precipitation Bias Correction (PBCOR) dataset, which is available online ().
引用
收藏
页码:1299 / 1315
页数:17
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