TY - JOUR
T1 - Bias correction of global high-resolution precipitation climatologies using streamflow observations from 9372 catchments
AU - Beck, Hylke E.
AU - Wood, Eric F.
AU - McVicar, Tim R.
AU - Zambrano-Bigiarini, Mauricio
AU - Alvarez-Garreton, Camila
AU - Baez-Villanueva, Oscar M.
AU - Sheffield, Justin
AU - Karger, Dirk N.
N1 - Generated from Scopus record by KAUST IRTS on 2023-02-14
PY - 2020/2/15
Y1 - 2020/2/15
N2 - We introduce a set of global high-resolution (0.058) 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 .608N, 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 yr21 (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 (http://www.gloh2o.org/pbcor/).
AB - We introduce a set of global high-resolution (0.058) 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 .608N, 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 yr21 (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 (http://www.gloh2o.org/pbcor/).
UR - https://journals.ametsoc.org/doi/10.1175/JCLI-D-19-0332.1
UR - http://www.scopus.com/inward/record.url?scp=85080054453&partnerID=8YFLogxK
U2 - 10.1175/JCLI-D-19-0332.1
DO - 10.1175/JCLI-D-19-0332.1
M3 - Article
SN - 0894-8755
VL - 33
SP - 1299
EP - 1315
JO - Journal of Climate
JF - Journal of Climate
IS - 4
ER -