Cold winter soils enhance dissolved organic carbon concentrations in soil and stream water

Concentrations of dissolved organic carbon ([DOC]) have increased in lakes, streams and rivers across a large part of the northern hemisphere and raised an animated scientific debate about the underlying mechanisms. The lack of consensus about the role of climate in controlling the DOC trends highli...

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Vydané v:	Geophysical research letters Ročník 37; číslo 8; s. np - n/a
Hlavní autori:	Haei, Mahsa, Öquist, Mats G., Buffam, Ishi, Ågren, Anneli, Blomkvist, Peder, Bishop, Kevin, Ottosson Löfvenius, Mikaell, Laudon, Hjalmar
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Washington, DC Blackwell Publishing Ltd 01.04.2010 American Geophysical Union John Wiley & Sons, Inc
Predmet:	Biogeochemistry Carbon Climate change Climatic conditions Cryosphere Dissolution Dissolved organic carbon Earth sciences Earth, ocean, space Environmental Sciences related to Agriculture and Land-use Exact sciences and technology Freshwater Geophysics Miljö- och naturvårdsvetenskap Moisture content Snowmelt soil frost Soil water Soils Streams Surface water Winter winter climate rivers trend-surface analysis springs streams latitude Summer concentration climate Dissolved organic carbon Dynamical climatology Climatic condition surface water Winter Northern Hemisphere gels Snow melt Spring(season) regulations Boreal lakes soils climate change
ISSN:	0094-8276, 1944-8007, 1944-8007
On-line prístup:	Získať plný text
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