Unterschiede
Hier werden die Unterschiede zwischen zwei Versionen angezeigt.
| Beide Seiten der vorigen Revision Vorhergehende Überarbeitung | |||
| thesis:link_spi_lowflow [2013/02/08 12:55] – kstahl | thesis:link_spi_lowflow [2013/12/15 20:42] (aktuell) – kstahl | ||
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| - | ====The linkage of meteorological drought indicators to low flow events across Europe==== | + | ====The linkage of meteorological drought indicators to low flow events across Europe |
| ==Background== | ==Background== | ||
| Extreme low flows have a number of negative impacts on ecology and economy. Operational monitoring and early warning of droughts, however, is mainly based on a number of different precipitation base drought indices such as the standardized precipitation index (SPI) and the standardized precipitation evaporation index (SPEI). An ongoing question is, how these meteorological indices are linked to drought in those components of the water cycle which allow direct use of the water, i.e. surface water (rivers and lakes) and groundwater. | Extreme low flows have a number of negative impacts on ecology and economy. Operational monitoring and early warning of droughts, however, is mainly based on a number of different precipitation base drought indices such as the standardized precipitation index (SPI) and the standardized precipitation evaporation index (SPEI). An ongoing question is, how these meteorological indices are linked to drought in those components of the water cycle which allow direct use of the water, i.e. surface water (rivers and lakes) and groundwater. | ||
| Zeile 18: | Zeile 18: | ||
| Vicente-Serrano, | Vicente-Serrano, | ||
| - | {{tag> | + | {{tag> |