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A young afforestation area in Iceland was a moderate sink to CO2 only a decade after scarification and establishment
A young afforestation area Iceland a decade after scarification and establishment
2010/1/21
This study reports on three years (2004–2006) of measurements of net ecosystem exchange (NEE) over a young Siberian larch plantation in Iceland established on previously grazed heathland pasture that ...
A rapid transition from ice covered CO2–rich waters to a biologically mediated CO2 sink in the eastern Weddell Gyre
rapid transition ice covered CO2–rich waters CO2 sink
2010/1/18
Circumpolar Deep Water (CDW), locally called Warm Deep Water (WDW), enters the Weddell Gyre in the southeast, roughly at 25° E to 30° E. In December 2002 and January 2003 we studied the effect of entr...
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania
Inter-annual variability carbon dioxide oceanic sink south of Tasmania
2010/1/15
We compiled a large data-set from 22 cruises spanning from 1991 to 2003, of the partial pressure of CO2 (pCO2) in surface waters over the continental shelf (CS) and adjacent open ocean (43° to 46° S; ...
An oceanic fixed nitrogen sink exceeding 400 Tg N a−1 vs the concept of homeostasis in the fixed-nitrogen inventory
oceanic fixed nitrogen sink concept of homeostasis fixed-nitrogen inventory
2010/1/14
Measurements of the N2 produced by denitrification, a better understanding of non-canonical pathways for N2 production such as the anammox reaction, better appreciation of the multiple environments in...
Link or sink:a modelling interpretation of the open Baltic biogeochemistry
Link sink modelling interpretation open Baltic biogeochemistry
2010/1/7
A 1-D model system, consisting of the 1-D version of the Princeton Ocean Model (POM) coupled with the European Regional Seas Ecosystem Model (ERSEM) has been applied to a sub-basin of the Baltic Prope...