Helmholtz-Zentrum Geesthacht

Institute for Coastal Research

Department of Paleoclimate


 
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Dpt. Paleoclimate

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Climate change?                     

                            It's always there!
New Multivariate Dataset HIRESAFF
Reconstruction of Higly Resolved Atmospheric Forcing Fields for NE-Europe since 1850 AD
We reconstructed a new dataset of spatio-temporal HIghly RESolved Atmospheric Forcing Fields (HIRESAFF) for Northern Europe since 1850. As an outcome of the BONUS project ECOSUPPORT, the reconstructed fields provide a new basis for ecosystem (or similar) models to run longer simulations also prior to a large human impact on the Baltic Sea. The dataset also allows a better validation and estimation of model uncertainties under different climatic or nutrient load conditions.

Domain NE-Europe, 71°N to 48°N / 5°W to 37°E
Domain for NE-Europe
Horizontal Resolution regular LatLon grid, 0.25° x 0.25°
Temporal Resolution daily, 1850-01-01 to 2009-09-29
Variables sea-surface pressure (SLP) [hPa]
zonal (U) and meridional (V) wind [m/s]
relative humidity (RH) [%]
total cloud cover (TCC) [%]
near-surface temperature (T2m) [K]
and precipitation (PREC) [mm]

Status: Official release within ECOSUPPORT, public release till end of 2011

The Analog-Method (AM) is used as a simple non-linear upscaling tool to reconstruct daily atmospheric fields from long historical station data of daily SLP and monthly T2m since 1850 (predictor). "Analogue" fields for every day (predictand) are searched by the AM from a pool of atmospheric fields taken from a regional climate model (1958-2007). As the AM is not assuming a specific shape for the probability distribution of the variables, non-normally as well as normally distributed variables are reconstructed. Hence, the AM reconstruction captures the extremes (magnitudes, frequencies), the probability distributions of the variables as well as the variability reasonably well on the daily scale.