Voorspelbaarheid neerslag winter met snow advance index

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Martijn
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Lid geworden op: Ma 1 Nov 2010, 21:56
Locatie: Gaasterland, Friesland

Voorspelbaarheid neerslag winter met snow advance index

Berichtdoor Martijn » Di 29 Okt 2013, 14:12

Onderstaande studie gaat over hoe de toename van de sneeuwbedekking van Eurazië in oktober, zoals beschreven in de recentelijk gepubliceerde snow advance index (SAI), gebruikt kan worden voor het voorspellen van de december–februari neerslag-totalen in Europa. Er zou sprake zijn van significante correlaties.

Bron: http://journals.ametsoc.org/doi/abs/10. ... 12-00083.1

Brands, S., R. Manzanas, J. M. Gutiérrez, J. Cohen, 2012: Seasonal Predictability of Wintertime Precipitation in Europe Using the Snow Advance Index. J. Climate, 25, 4023–4028.
doi: http://dx.doi.org/10.1175/JCLI-D-12-00083.1

Seasonal Predictability of Wintertime Precipitation in Europe Using the Snow Advance Index

S. Brands, R. Manzanas, and J. M. Gutiérrez
Instituto de Física de Cantabria (CSIC-UC), Santander, Spain

J. Cohen
Atmospheric and Environmental Research, Lexington, Massachusetts

Abstract

This study tests the applicability of Eurasian snow cover increase in October, as described by the recently published snow advance index (SAI), for forecasting December–February precipitation totals in Europe.

On the basis of a classical correlation analysis, global significance was obtained and locally significant correlation coefficients of up to 0.89 and −0.78 were found for the Iberian Peninsula and southern Norway, respectively.

For a more robust assessment of these results, a linear regression approach is followed to hindcast the precipitation sums in a 1-yr-out cross-validation framework, using the SAI as the only predictor variable.

With this simple empirical approach, local-scale precipitation could be reproduced with a correlation of up to 0.84 and 0.71 for the Iberian Peninsula and southern Norway, respectively, while catchment aggregations on the Iberian Peninsula could be hindcast with a correlation of up to 0.73.

These findings are confirmed when repeating the hindcast approach to a degraded but much longer version of the SAI.

With the recommendation to monitor the robustness of these results as the sample size of the SAI increases, the authors encourage its use for the purpose of seasonal forecasting in southern Norway and the Iberian Peninsula, where general circulation models are known to perform poorly for the variable in question.

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