Coupling Terrestrial and Atmospheric Water Dynamics to Improve Prediction in a Changing Environment

At shorter time scales, heterogeneous patterns in precipitation drive spatial variability in soil moisture, which potentially impacts hydrologic responses from future storm events.\n As seen in recent experiments in the Niwot Ridge Long Term Ecological Research (LTER) site, lengthening of the growin...

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Veröffentlicht in:	Bulletin of the American Meteorological Society 2008-09, Vol.89 (9), p.1275-1279
Hauptverfasser:	Lyon, Steve W., Dominguez, Francina, Gochis, David J., Brunsell, Nathaniel A., Castro, Christopher L., Chow, Fotini K., Fan, Ying, Fuka, Daniel, Hong, Yang, Kucera, Paul A., Nesbitt, Stephen W., Salzmann, Nadine, Schmidli, Juerg, Snyder, Peter K., Teuling, Adriaan J., Twine, Tracy E., Levis, Samuel, Lundquist, Jessica D., Salvucci, Guido D., Sealy, Andrea M., Walter, M. Todd
Format:	Artikel
Sprache:	eng
Schlagworte:	Atmospheric circulation Atmospheric models Atmospheric water Atmospherics Climate models Climatic zones Data assimilation Ecological research Environmental changes Evapotranspiration Groundwater Growing season Hydrological modeling IN BOX INSIGHTS and INNOVATIONS Meteorology Monitoring systems Soil atmosphere interactions Soil moisture Soil water Studies Vegetation Water cycle
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Beschreibung
Zusammenfassung:	At shorter time scales, heterogeneous patterns in precipitation drive spatial variability in soil moisture, which potentially impacts hydrologic responses from future storm events.\n As seen in recent experiments in the Niwot Ridge Long Term Ecological Research (LTER) site, lengthening of the growing season significantly alters the seasonal timing of groundwater extraction and canopy fluxes of moisture and carbon.
ISSN:	0003-0007 1520-0477
DOI:	10.1175/2008BAMS2547.1