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Conradt, T., Hattermann, F. F., Koch, H., & Wechsung, F. (2013). Klima- und Landnutzungsszenarien in ihren Wirkungen auf den Wasserabfluss. In F. Wechsung, V. Hartje, S. Kaden, M. Venohr, B. Hansjürgens, & P. Gräfe (Eds.), (pp. 177–209). Die Elbe im globalen Wandel. Berlin: Weißensee Verl.
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Conradt, T., Koch, H., Hattermann, F. F., Wechsung, F., Hartje, V., Kaden, S., et al. (2013). Validierung von Lokalkorrekturen der Verdunstung bei den Simulationen des Wasserabflusses. In F. Wechsung, V. Hartje, S. Kaden, M. Venohr, B. Hansjürgens, & P. Gräfe (Eds.), (pp. 211–231). Die Elbe im globalen Wandel. Berlin: Weißensee Verl.
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Bussel, V., Ewert, F., & et al. Spatial sampling of weather data for regional crop yield simulations.
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Boote, K. J., Porter, C., Jones, J. W., Thorburn, P. J., Kersebaum, K. C., Hoogenboom, G., et al. (2015). Sentinel site data for crop model improvement – definition and characterization. In J. L. Hatfield, & D. Fleisher (Eds.), (Vol. Advances in Agricultural Systems Modeling (7)). Madison, WI: ASA, CSSA, and SSSA.
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Semenov, M. A., & Stratonovitch, P. (2016). Local-scale CMIP5-based climate scenarios for MACSUR2 (Vol. 8).
Abstract: Climate sensitivity of GCMs was used to select 5 GCMs from the CMIP5 ensemble for impact studies in MACSUR2. Selected GCMs for MACSUR2 are EC-EARTH (7), GFDL-CM3 (8) HadGEM2-ES (10), MIROC5 (13), and MPI-ESM-MR (15). These GCMs are evenly distributed among CMIP5 (Fig 1) and should capture, in principal, climate uncertainty of the CMIP5 ensemble. Using 5 GCMs will enable us to assess uncertainties in impacts related to uncertainty in climate projections. The selection of GCMs in MACSUR2 has a good overlap with selections of GCMs used in CORDEX and AgMIP projects. We used the LARS-WG generator to construct local-scale CMIP5-based climate scenarios for Europe (Semenov & Stratonovitch, 2015). Fifteen sites were selected in Europe for MACSUR2. For each site and each selected GCM, 100 yrs climate daily data were generated by LARS-WG for RCP4.5 and RCP8.5 emission scenarios and for baseline and 3 future periods: near-term (2021-2040), mid-term (2041-2060) and long-term (2081-2100).
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