Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Catchment-scale thawing and greening decreases long-term nitrogen export in NE Greenland
Climate change is expected to alter nitrogen (N) export from Arctic rivers, with potential implications for fragile coastal ecosystems and fisheries. Yet, the directionality of change is poorly understood, as increased mobilization of N in a ‘thawing’ Arctic is countered by higher rates of vegetative uptake in a ‘greening’ Arctic, particularly in the understudied region of Greenland. We use an unprecedented dataset of long-term ( n = 18 years) river chemistry, streamflow, and catchment-scale changes in snow and vegetation to document changing riverine N loss in Greenland. We documented decreasing inorganic and organic N loads, linked to decreasing snow stores, warming soils, and enhanced plant uptake. Higher variability in N export across years also points to the increasing role of high flow events in driving downstream N loss. This alteration in N cycling may significantly reduce both inorganic and organic N transport across the terrestrial-aquatic boundary during the open water season in a rapidly warming Greenland.
Catchment-scale thawing and greening decreases long-term nitrogen export in NE Greenland
Climate change is expected to alter nitrogen (N) export from Arctic rivers, with potential implications for fragile coastal ecosystems and fisheries. Yet, the directionality of change is poorly understood, as increased mobilization of N in a ‘thawing’ Arctic is countered by higher rates of vegetative uptake in a ‘greening’ Arctic, particularly in the understudied region of Greenland. We use an unprecedented dataset of long-term ( n = 18 years) river chemistry, streamflow, and catchment-scale changes in snow and vegetation to document changing riverine N loss in Greenland. We documented decreasing inorganic and organic N loads, linked to decreasing snow stores, warming soils, and enhanced plant uptake. Higher variability in N export across years also points to the increasing role of high flow events in driving downstream N loss. This alteration in N cycling may significantly reduce both inorganic and organic N transport across the terrestrial-aquatic boundary during the open water season in a rapidly warming Greenland.
Catchment-scale thawing and greening decreases long-term nitrogen export in NE Greenland
Shannon L Speir (Autor:in) / Jennifer L Tank (Autor:in) / Ada Pastor (Autor:in) / Marc F Muller (Autor:in) / Mikhail Mastepanov (Autor:in) / Tenna Riis (Autor:in)
2024
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Metadata by DOAJ is licensed under CC BY-SA 1.0
Catchment "greening" using stormwater in Adelaide, South Australia
British Library Conference Proceedings | 1999
|Catchment controls on solute export
British Library Online Contents | 2015
|Catchment controls on solute export
British Library Online Contents | 2015
|Long- and Short-Term Inorganic Nitrogen Runoff from a Karst Catchment in Austria
DOAJ | 2020
|