Opis projektu
Lód morski na północno-zachodnim Atlantyku i jego rola w procesie rozpadu lądolodów
Jaka jest rola lodu morskiego w systemie klimatycznym? Czy obecny ubytek lodu morskiego ma wpływ na lądolód grenlandzki? Odpowiedź na te pytania polega na zrozumieniu reakcji lądolodów na zmiany klimatu w przeszłości. Celem finansowanego ze środków UE projektu IceLab w tym zakresie jest zbadanie związku między lodem morskim, prądami morskimi, ociepleniem podpowierzchniowym i rozpadem lądolodu na Morzu Labradorskim. Nacisk kładziony jest na zrozumienie znaczenia lodu morskiego dla stabilności lądolodu. Metodologia oparta będzie na zintegrowanym podejściu geochemii organicznej i nieorganicznej w połączeniu z najnowocześniejszymi technikami datowania i korelacji. Ostatecznie projekt przyczyni się do poprawy sposobu prognozowania utraty masy lądolodu grenlandzkiego.
Cel
Northern hemisphere ice sheets are particularly vulnerable to climate change as the Arctic is warming twice as fast as the rest of the planet. Scenarios of future ice sheet stability, however, are associated with significant uncertainty, due to a lack of understanding of the relevant internal climate feedbacks. These processes involve ocean-ice sheet interactions and the effects of sea ice on the terrestrial cryosphere. With increased societal concerns over rising sea levels, it is more than ever important to understand the implications of climate change for ice sheet stability. The key lies in understanding the response of past ice sheets to climate change.
Prominent episodes of past ice-sheet collapse are so-called Heinrich events during the last glacial period, originating in Hudson Strait. While modelling studies have long hinted at the importance of sea ice in the Labrador Sea for subsurface warming and ocean induced melting during Heinrich events, this has not been shown using proxy methods. My project will investigate the links and feedbacks of sea ice, ocean circulation, subsurface warming, and ice-sheet collapse in the Labrador Sea to determine the role of the coupled cryosphere-ocean system for ice sheet stability across. Additionally, the effect of enhanced freshwater discharge on the system will be documented and a spatial-temporal map of North Atlantic sea ice dynamics across Heinrich events will be constructed. I will apply an integrated approach of organic and inorganic geochemistry, using sea-ice biomarkers, foraminiferal isotopes, and foraminiferal trace metals (i.e. Mg/Ca) in combination with state-of-the-art dating and correlation techniques. The new records will provide important clues with respect to a potential oceanic trigger of Hudson Strait iceberg surges during Heinrich events as well as advancing our understanding of the coupled cryosphere-ocean system, vital to accurately predict mass loss from the Greenland ice sheet in the future.
Dziedzina nauki
- natural sciencesearth and related environmental sciencesgeochemistry
- natural sciencesphysical sciencesastronomyplanetary sciencesplanets
- natural sciencesearth and related environmental sciencesatmospheric sciencesclimatologyclimatic changes
- natural sciencesearth and related environmental sciencesphysical geographyglaciology
Słowa kluczowe
Program(-y)
Temat(-y)
System finansowania
MSCA-IF - Marie Skłodowska-Curie Individual Fellowships (IF)Koordynator
8000 Aarhus C
Dania