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  • 1
    Publication Date: 2024-02-28
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉High spatio‐temporal resolution near‐surface projected data is vital for climate change impact studies and adaptation. We derived the highest statistically downscaled resolution multivariate ensemble currently available: daily 1 km until the end of the century. Deep learning models were employed to develop transfer functions for precipitation, water vapor pressure, radiation, wind speed, and, maximum, mean and minimum temperature. Perfect prognosis is the particular statistical downscaling methodology applied, using a subset of the ReKIS data set for Saxony as predictands, the ERA5 reanalysis as during‐training predictors and the CORDEX‐EUR11 ensemble as projected predictors. The performance of the transfer functions was validated with the VALUE framework, yielding highly satisfactory results. Particular attention was given to the three major perfect prognosis assumptions, for which several tests were carried out and thoroughly discussed. From the latter, we corroborated their fulfillment to a high degree, thus, the derived projections are considered adequate and relevant for impact modelers. In total, 18 runs for RCP85, 1 for RCP45, and 4 for RCP26 were downscaled under both stochastic and deterministic approaches. This multivariate ensemble could drive more accurate and diverse impact studies in the region. Generally, the projected climatologies are in agreement with coarser resolution projections. Nevertheless, statistical particularities were observed for some projections, thus, a list of caveats for potential users is given. Due to the scalability of the presented methodology, further possible applications with additional datasets are proposed. Lastly, several potential improvement prospects are discussed toward the ideal subsequent iteration of the perfect prognosis statistical downscaling methodology.〈/p〉
    Description: Plain Language Summary: There is a great worldwide demand for high spatio‐temporal resolution projections to develop climate change adaptation and mitigation schemes. Despite recent improvements, the resolution of both global and regional climate models is still too coarse to properly represent local variability, particularly in complex terrains. Depending on the application, impact modelers and decision makers require kilometer‐scale projections, with a minimum daily temporal resolution, of near‐surface variables. To fill this information gap, we employed artificial intelligence algorithms to downscale, to a novel daily 1 km resolution, a projection ensemble until the end of the century consisting of precipitation, water vapor pressure, radiation, wind speed, and, maximum, mean and minimum temperature. The ensemble comprises 18 runs of the business‐as‐usual worst‐case scenario (RCP85), 1 run of the stabilization scenario (RCP45), and 4 of the optimistic low‐emissions scenario (RCP26). The main assumptions of the methodology were thoroughly tested and discussed. The validation carried out yielded highly satisfactory results. Thus, we consider the projections to be adequate and relevant for impact studies. The region studied is located in Saxony (Germany), still, the methodology shown is potentially applicable anywhere in the world.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Highest statistically downscaled spatio‐temporal resolution multivariate ensemble currently available, consisting of 23 projection runs〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉We downscaled precipitation, water vapor pressure, radiation, wind speed, and, maximum, mean and minimum temperature〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The methodology complied to a high degree with the three perfect prognosis assumptions and is scalable to other spatio‐temporal resolutions〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: European Social Fund, Freistaat Sachsen http://dx.doi.org/10.13039/501100004895
    Description: https://rekis.hydro.tu-dresden.de/
    Description: https://doi.org/10.5281/zenodo.7570247
    Description: https://doi.org/10.5281/zenodo.7559173
    Description: https://doi.org/10.5281/zenodo.7558945
    Description: https://doi.org/10.5281/zenodo.8059248
    Description: https://doi.org/10.5281/zenodo.8198925
    Keywords: ddc:551.6 ; climate change ; statistical downscaling ; perfect prognosis ; ERA5 ; CORDEX ; deep learning ; multivariate ensemble
    Language: English
    Type: doc-type:article
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  • 2
    Publication Date: 2021-10-07
    Description: Land use and climate changes both affect terrestrial ecosystems. Here, we used three combinations of Shared Socioeconomic Pathways and Representative Concentration Pathways (SSP1xRCP26, SSP3xRCP60, and SSP5xRCP85) as input to three dynamic global vegetation models to assess the impacts and associated uncertainty on several ecosystem functions: terrestrial carbon storage and fluxes, evapotranspiration, surface albedo, and runoff. We also performed sensitivity simulations in which we kept either land use or climate (including atmospheric CO2) constant from year 2015 on to calculate the isolated land use versus climate effects. By the 2080–2099 period, carbon storage increases by up to 87 ± 47 Gt (SSP1xRCP26) compared to present day, with large spatial variance across scenarios and models. Most of the carbon uptake is attributed to drivers beyond future land use and climate change, particularly the lagged effects of historic environmental changes. Future climate change typically increases carbon stocks in vegetation but not soils, while future land use change causes carbon losses, even for net agricultural abandonment (SSP1xRCP26). Evapotranspiration changes are highly variable across scenarios, and models do not agree on the magnitude or even sign of change of the individual effects. A calculated decrease in January and July surface albedo (up to −0.021 ± 0.007 and −0.004 ± 0.004 for SSP5xRCP85) and increase in runoff (+67 ± 6 mm/year) is largely driven by climate change. Overall, our results show that future land use and climate change will both have substantial impacts on ecosystem functioning. However, future changes can often not be fully explained by these two drivers and legacy effects have to be considered.
    Keywords: 333.7 ; 551.6 ; land use change ; climate change projections ; terrestrial ecosystems ; vegetation modeling ; ecosystem service indicators ; legacy effects
    Language: English
    Type: map
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  • 3
    Publication Date: 2004
    Keywords: Geochemistry ; Seismicity ; Borehole geophys. ; Volcanology ; PAG ; Fernandez ; Vinas ; Sanchez ; Martin ; Nuez ; Almazan
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  • 4
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    U.S. Geol. Surv., Prof. Pap.
    In:  Professional Paper, The Guatemalan Earthquake of February 4, 1976, A Preliminary Report, Dordrecht, xvii+329 pp., U.S. Geol. Surv., Prof. Pap., vol. 1002, no. 231, pp. 52-66, (ISBN 1-4020-1729-4)
    Publication Date: 1976
    Keywords: Earthquake ; Source parameters ; Intensity
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