On the procurement of physical risk assessments for climate-related disclosures: guidance from a climate science perspective. [PDF]
Harrington LJ +5 more
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Hybrid physical-statistical framework for seasonal streamflow forecasting in the Upper Feather River Basin, California. [PDF]
Ozcan Z +7 more
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Projections of temperature and precipitation changes in Xinjiang from 2021 to 2050 based on the CMIP6 model. [PDF]
Zhang Y, Zhang P, Gu X, Long A.
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Convolutional Long Short-Term Memory network for generating 100 m daily near-surface air temperature. [PDF]
Sun M +6 more
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The Ouranos CRCM5-CMIP6 ensemble: A dynamically downscaled ensemble of CMIP6 simulations over North America. [PDF]
Paquin D +7 more
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Statistical Downscaling over Italy using EQM: CMIP6 Climate Projections for the 1985-2100 Period. [PDF]
Fedele G, Reder A, Mercogliano P.
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AbstractDownscaling is a fundamental procedure in the assessment of the future climate change impact at regional and watershed scales. Hence, it is important to investigate the spatial variability of the climate conditions that are constructed by various downscaling methods to assess whether each method can properly model the climate conditions at ...
S. Jang, M. L. Kavvas
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Statistical-dynamical downscaling of wind climatologies
Journal of Wind Engineering and Industrial Aerodynamics, 1997Abstract A statistical-dynamical downscaling procedure is applied for an investigation into the availability of wind power over a region of 80 × 87 km which covers flat and hilly terrain. The approach is based on the statistical coupling of a regionally representative wind climate with a numerical atmospheric mesoscale model.
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Downscaling from GCM precipitation: a benchmark for dynamical and statistical downscaling methods
International Journal of Climatology, 2006A precipitation downscaling method is presented using precipitation from a general circulation model (GCM) as predictor. The method extends a previous method from monthly to daily temporal resolution. The simplest form of the method corrects for biases in wet-day frequency and intensity. A more sophisticated variant also takes account of flow-dependent
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