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High-resolution (1 km) Köppen-Geiger maps for 1901-2099 based on constrained CMIP6 projections.
Beck, Hylke E; McVicar, Tim R; Vergopolan, Noemi; Berg, Alexis; Lutsko, Nicholas J; Dufour, Ambroise; Zeng, Zhenzhong; Jiang, Xin; van Dijk, Albert I J M; Miralles, Diego G.
Afiliación
  • Beck HE; King Abdullah University of Science and Technology, Thuwal, Saudi Arabia. hylke.beck@gmail.com.
  • McVicar TR; CSIRO Environment, Canberra, ACT, Australia.
  • Vergopolan N; Australian Research Council Centre of Excellence for Climate Extremes, Canberra, ACT, Australia.
  • Berg A; Atmospheric and Ocean Sciences Program, Princeton University, Princeton, New Jersey, USA.
  • Lutsko NJ; NOAA Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey, USA.
  • Dufour A; University of Montreal, Montreal, Quebec, Canada.
  • Zeng Z; Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA.
  • Jiang X; King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.
  • van Dijk AIJM; School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China.
  • Miralles DG; School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, China.
Sci Data ; 10(1): 724, 2023 10 23.
Article en En | MEDLINE | ID: mdl-37872197
ABSTRACT
We introduce Version 2 of our widely used 1-km Köppen-Geiger climate classification maps for historical and future climate conditions. The historical maps (encompassing 1901-1930, 1931-1960, 1961-1990, and 1991-2020) are based on high-resolution, observation-based climatologies, while the future maps (encompassing 2041-2070 and 2071-2099) are based on downscaled and bias-corrected climate projections for seven shared socio-economic pathways (SSPs). We evaluated 67 climate models from the Coupled Model Intercomparison Project phase 6 (CMIP6) and kept a subset of 42 with the most plausible CO2-induced warming rates. We estimate that from 1901-1930 to 1991-2020, approximately 5% of the global land surface (excluding Antarctica) transitioned to a different major Köppen-Geiger class. Furthermore, we project that from 1991-2020 to 2071-2099, 5% of the land surface will transition to a different major class under the low-emissions SSP1-2.6 scenario, 8% under the middle-of-the-road SSP2-4.5 scenario, and 13% under the high-emissions SSP5-8.5 scenario. The Köppen-Geiger maps, along with associated confidence estimates, underlying monthly air temperature and precipitation data, and sensitivity metrics for the CMIP6 models, can be accessed at www.gloh2o.org/koppen .

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Sci Data Año: 2023 Tipo del documento: Article País de afiliación: Arabia Saudita

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Idioma: En Revista: Sci Data Año: 2023 Tipo del documento: Article País de afiliación: Arabia Saudita