Arctic marine systems are vital to the Earth’s ecological and climatic balance and harbour a unique biodiversity adapted to extreme conditions. However, they are under unprecedented threat from climate change, in particular from “Atlantification”, i.e., the loss of sea ice and the increasing influence of Atlantic Water (AW) in this region. Long-term observatories are crucial to detect even small changes in these dynamic ecosystems. Svalbard, with its easily accessible infrastructure, is a strategic location for studying these changes. We have identified marine time series that clearly illustrate the signature of Atlantification in the Svalbard region over the last two decades. These time series provide insight into the propagation of AW and the interaction between the continental slope, the shelf and the fjord systems. Seasonal and multi-year temperature and salinity patterns illustrate the varying influence of AW, with long-term variability showing, among others, a freshening phase since 2018, possibly related to North Atlantic freshwater anomalies.

The Atlantification process in Svalbard: a broad view from the SIOS Marine Infrastructure Network (ARiS)

Manuel Bensi
Primo
Supervision
;
Francesco Paladini de Mendoza;Gianmarco Ingrosso;Leonardo Langone;Patrizia Giordano;
2024

Abstract

Arctic marine systems are vital to the Earth’s ecological and climatic balance and harbour a unique biodiversity adapted to extreme conditions. However, they are under unprecedented threat from climate change, in particular from “Atlantification”, i.e., the loss of sea ice and the increasing influence of Atlantic Water (AW) in this region. Long-term observatories are crucial to detect even small changes in these dynamic ecosystems. Svalbard, with its easily accessible infrastructure, is a strategic location for studying these changes. We have identified marine time series that clearly illustrate the signature of Atlantification in the Svalbard region over the last two decades. These time series provide insight into the propagation of AW and the interaction between the continental slope, the shelf and the fjord systems. Seasonal and multi-year temperature and salinity patterns illustrate the varying influence of AW, with long-term variability showing, among others, a freshening phase since 2018, possibly related to North Atlantic freshwater anomalies.
2024
Istituto di Scienze Polari - ISP - Sede Secondaria Bologna
Istituto di Scienze Polari - ISP - sede Secondaria Messina
Istituto di Ricerca sugli Ecosistemi Terrestri - IRET
978-82-93871-14-9
Fram Strait
climate change
marine network
long-term changes
Atlantification
Svalbard fjords
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/537207
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