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The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover. / Dahlke, Sandro; Hughes, Nicholas Edward ; Mae Wagner, Penelope ; Gerland, Sebastian ; Wawrzyniak, Tomasz ; Иванов, Борис Вячеславович; Maturilli, Marion.

In: International Journal of Climatology, Vol. 40, No. 12, 01.10.2020, p. 5246-5265.

Research output: Contribution to journalArticlepeer-review

Harvard

Dahlke, S, Hughes, NE, Mae Wagner, P, Gerland, S, Wawrzyniak, T, Иванов, БВ & Maturilli, M 2020, 'The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover', International Journal of Climatology, vol. 40, no. 12, pp. 5246-5265. https://doi.org/10.1002/joc.6517

APA

Dahlke, S., Hughes, N. E., Mae Wagner, P., Gerland, S., Wawrzyniak, T., Иванов, Б. В., & Maturilli, M. (2020). The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover. International Journal of Climatology, 40(12), 5246-5265. https://doi.org/10.1002/joc.6517

Vancouver

Dahlke S, Hughes NE, Mae Wagner P, Gerland S, Wawrzyniak T, Иванов БВ et al. The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover. International Journal of Climatology. 2020 Oct 1;40(12):5246-5265. https://doi.org/10.1002/joc.6517

Author

Dahlke, Sandro ; Hughes, Nicholas Edward ; Mae Wagner, Penelope ; Gerland, Sebastian ; Wawrzyniak, Tomasz ; Иванов, Борис Вячеславович ; Maturilli, Marion. / The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover. In: International Journal of Climatology. 2020 ; Vol. 40, No. 12. pp. 5246-5265.

BibTeX

@article{6c20f67f7ea24f54a015d483e3f8e7fd,
title = "The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover",
abstract = "The Svalbard archipelago in the Arctic North Atlantic is experiencing rapid changes in the surface climate and sea ice distribution, with impacts for the coupled climate system and the local society. This study utilizes observational data of surface air temperature (SAT) from 1980–2016 across the whole Svalbard archipelago, and sea ice extent (SIE) from operational sea ice charts to conduct a systematic assessment of climatologies, long‐term changes and regional differences. The proximity to the warm water mass of the West Spitsbergen Current drives a markedly warmer climate in the western coastal regions compared to northern and eastern Svalbard. This imprints on the SIE climatology in southern and western Svalbard, where the annual maxima of 50–60% area ice coverage are substantially less than 80–90% in the northern and eastern fjords. Owing to winter‐amplified warming, the local climate is shifting towards more maritime conditions, and SIE reductions of between 5 and 20% per decade in particular regions are found, such that a number of fjords in the west have been virtually ice‐free in recent winters. The strongest decline comes along with SAT forcing and occurs over the most recent 1–2 decades in all regions; while in the 1980s and 1990s, enhanced northerly winds and sea ice drift can explain 30–50% of SIE variability around northern Svalbard, where they had correspondingly lead to a SIE increase. With an ongoing warming it is suggested that both the meteorological and cryospheric conditions in eastern Svalbard will become increasingly similar to what is already observed in the western fjords, namely suppressed typical Arctic climate conditions.",
keywords = "Arctic warming, climatology, observations, sea ice, surface meteorology, Svalbard, ARCTIC AMPLIFICATION, ATMOSPHERIC CIRCULATION, ATLANTIC WATER, THICKNESS, VARIABILITY, CLIMATE, KONGSFJORDEN, TRENDS, EXTENT, NORTH",
author = "Sandro Dahlke and Hughes, {Nicholas Edward} and {Mae Wagner}, Penelope and Sebastian Gerland and Tomasz Wawrzyniak and Иванов, {Борис Вячеславович} and Marion Maturilli",
note = "Publisher Copyright: {\textcopyright} 2020 The Authors. International Journal of Climatology published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society.",
year = "2020",
month = oct,
day = "1",
doi = "10.1002/joc.6517",
language = "English",
volume = "40",
pages = "5246--5265",
journal = "International Journal of Climatology",
issn = "0899-8418",
publisher = "Wiley-Blackwell",
number = "12",

}

RIS

TY - JOUR

T1 - The observed recent surface air temperature development across Svalbard and concurring footprints in local sea ice cover

AU - Dahlke, Sandro

AU - Hughes, Nicholas Edward

AU - Mae Wagner, Penelope

AU - Gerland, Sebastian

AU - Wawrzyniak, Tomasz

AU - Иванов, Борис Вячеславович

AU - Maturilli, Marion

N1 - Publisher Copyright: © 2020 The Authors. International Journal of Climatology published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society.

PY - 2020/10/1

Y1 - 2020/10/1

N2 - The Svalbard archipelago in the Arctic North Atlantic is experiencing rapid changes in the surface climate and sea ice distribution, with impacts for the coupled climate system and the local society. This study utilizes observational data of surface air temperature (SAT) from 1980–2016 across the whole Svalbard archipelago, and sea ice extent (SIE) from operational sea ice charts to conduct a systematic assessment of climatologies, long‐term changes and regional differences. The proximity to the warm water mass of the West Spitsbergen Current drives a markedly warmer climate in the western coastal regions compared to northern and eastern Svalbard. This imprints on the SIE climatology in southern and western Svalbard, where the annual maxima of 50–60% area ice coverage are substantially less than 80–90% in the northern and eastern fjords. Owing to winter‐amplified warming, the local climate is shifting towards more maritime conditions, and SIE reductions of between 5 and 20% per decade in particular regions are found, such that a number of fjords in the west have been virtually ice‐free in recent winters. The strongest decline comes along with SAT forcing and occurs over the most recent 1–2 decades in all regions; while in the 1980s and 1990s, enhanced northerly winds and sea ice drift can explain 30–50% of SIE variability around northern Svalbard, where they had correspondingly lead to a SIE increase. With an ongoing warming it is suggested that both the meteorological and cryospheric conditions in eastern Svalbard will become increasingly similar to what is already observed in the western fjords, namely suppressed typical Arctic climate conditions.

AB - The Svalbard archipelago in the Arctic North Atlantic is experiencing rapid changes in the surface climate and sea ice distribution, with impacts for the coupled climate system and the local society. This study utilizes observational data of surface air temperature (SAT) from 1980–2016 across the whole Svalbard archipelago, and sea ice extent (SIE) from operational sea ice charts to conduct a systematic assessment of climatologies, long‐term changes and regional differences. The proximity to the warm water mass of the West Spitsbergen Current drives a markedly warmer climate in the western coastal regions compared to northern and eastern Svalbard. This imprints on the SIE climatology in southern and western Svalbard, where the annual maxima of 50–60% area ice coverage are substantially less than 80–90% in the northern and eastern fjords. Owing to winter‐amplified warming, the local climate is shifting towards more maritime conditions, and SIE reductions of between 5 and 20% per decade in particular regions are found, such that a number of fjords in the west have been virtually ice‐free in recent winters. The strongest decline comes along with SAT forcing and occurs over the most recent 1–2 decades in all regions; while in the 1980s and 1990s, enhanced northerly winds and sea ice drift can explain 30–50% of SIE variability around northern Svalbard, where they had correspondingly lead to a SIE increase. With an ongoing warming it is suggested that both the meteorological and cryospheric conditions in eastern Svalbard will become increasingly similar to what is already observed in the western fjords, namely suppressed typical Arctic climate conditions.

KW - Arctic warming

KW - climatology

KW - observations

KW - sea ice

KW - surface meteorology

KW - Svalbard

KW - ARCTIC AMPLIFICATION

KW - ATMOSPHERIC CIRCULATION

KW - ATLANTIC WATER

KW - THICKNESS

KW - VARIABILITY

KW - CLIMATE

KW - KONGSFJORDEN

KW - TRENDS

KW - EXTENT

KW - NORTH

UR - http://www.scopus.com/inward/record.url?scp=85083061058&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/8e67376f-aef9-3b89-ae52-6472838c951f/

U2 - 10.1002/joc.6517

DO - 10.1002/joc.6517

M3 - Article

VL - 40

SP - 5246

EP - 5265

JO - International Journal of Climatology

JF - International Journal of Climatology

SN - 0899-8418

IS - 12

ER -

ID: 53665058