Hotspots and key periods of Greenland climate change during the past six decades

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Standard

Hotspots and key periods of Greenland climate change during the past six decades. / Abermann, Jakob; Hansen, Birger; Lund, Magnus; Wacker, Stefan; Karami, Mojtaba; Cappelen, John.

I: Ambio, Bind 46, Nr. Suppl. 1, 2017, s. 3-11.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Abermann, J, Hansen, B, Lund, M, Wacker, S, Karami, M & Cappelen, J 2017, 'Hotspots and key periods of Greenland climate change during the past six decades', Ambio, bind 46, nr. Suppl. 1, s. 3-11. https://doi.org/10.1007/s13280-016-0861-y

APA

Abermann, J., Hansen, B., Lund, M., Wacker, S., Karami, M., & Cappelen, J. (2017). Hotspots and key periods of Greenland climate change during the past six decades. Ambio, 46(Suppl. 1), 3-11. https://doi.org/10.1007/s13280-016-0861-y

Vancouver

Abermann J, Hansen B, Lund M, Wacker S, Karami M, Cappelen J. Hotspots and key periods of Greenland climate change during the past six decades. Ambio. 2017;46(Suppl. 1):3-11. https://doi.org/10.1007/s13280-016-0861-y

Author

Abermann, Jakob ; Hansen, Birger ; Lund, Magnus ; Wacker, Stefan ; Karami, Mojtaba ; Cappelen, John. / Hotspots and key periods of Greenland climate change during the past six decades. I: Ambio. 2017 ; Bind 46, Nr. Suppl. 1. s. 3-11.

Bibtex

@article{f8fcc624f8be4f9cbef26592e20b6b49,
title = "Hotspots and key periods of Greenland climate change during the past six decades",
abstract = "We investigated air temperature and pressure gradients and their trends for the period 1996–2014 in Greenland and compared these to other periods since 1958. Both latitudinal temperature and pressure gradients were strongest during winter. An overall temperature increase up to 0.15 °C year−1 was observed for 1996–2014. The strongest warming happened during February at the West coast (up to 0.6 °C year−1), weaker but consistent and significant warming occurred during summer months (up to 0.3 °C year−1) both in West and East Greenland. Pressure trends on a monthly basis were mainly negative, but largely statistically non-significant. Compared with other time windows in the past six decades, the period 1996–2014 yielded an above-average warming trend. Northeast Greenland and the area around Zackenberg follow the general pattern but are on the lower boundary of observed significant trends in Greenland. We conclude that temperature-driven ecosystem changes as observed in Zackenberg may well be exceeded in other areas of Greenland.",
keywords = "Air pressure trends, Ecosystem changes, Greenland climate change, Temperature trends",
author = "Jakob Abermann and Birger Hansen and Magnus Lund and Stefan Wacker and Mojtaba Karami and John Cappelen",
note = "CENPERMOA[2017]",
year = "2017",
doi = "10.1007/s13280-016-0861-y",
language = "English",
volume = "46",
pages = "3--11",
journal = "Ambio",
issn = "0044-7447",
publisher = "Springer",
number = "Suppl. 1",

}

RIS

TY - JOUR

T1 - Hotspots and key periods of Greenland climate change during the past six decades

AU - Abermann, Jakob

AU - Hansen, Birger

AU - Lund, Magnus

AU - Wacker, Stefan

AU - Karami, Mojtaba

AU - Cappelen, John

N1 - CENPERMOA[2017]

PY - 2017

Y1 - 2017

N2 - We investigated air temperature and pressure gradients and their trends for the period 1996–2014 in Greenland and compared these to other periods since 1958. Both latitudinal temperature and pressure gradients were strongest during winter. An overall temperature increase up to 0.15 °C year−1 was observed for 1996–2014. The strongest warming happened during February at the West coast (up to 0.6 °C year−1), weaker but consistent and significant warming occurred during summer months (up to 0.3 °C year−1) both in West and East Greenland. Pressure trends on a monthly basis were mainly negative, but largely statistically non-significant. Compared with other time windows in the past six decades, the period 1996–2014 yielded an above-average warming trend. Northeast Greenland and the area around Zackenberg follow the general pattern but are on the lower boundary of observed significant trends in Greenland. We conclude that temperature-driven ecosystem changes as observed in Zackenberg may well be exceeded in other areas of Greenland.

AB - We investigated air temperature and pressure gradients and their trends for the period 1996–2014 in Greenland and compared these to other periods since 1958. Both latitudinal temperature and pressure gradients were strongest during winter. An overall temperature increase up to 0.15 °C year−1 was observed for 1996–2014. The strongest warming happened during February at the West coast (up to 0.6 °C year−1), weaker but consistent and significant warming occurred during summer months (up to 0.3 °C year−1) both in West and East Greenland. Pressure trends on a monthly basis were mainly negative, but largely statistically non-significant. Compared with other time windows in the past six decades, the period 1996–2014 yielded an above-average warming trend. Northeast Greenland and the area around Zackenberg follow the general pattern but are on the lower boundary of observed significant trends in Greenland. We conclude that temperature-driven ecosystem changes as observed in Zackenberg may well be exceeded in other areas of Greenland.

KW - Air pressure trends

KW - Ecosystem changes

KW - Greenland climate change

KW - Temperature trends

U2 - 10.1007/s13280-016-0861-y

DO - 10.1007/s13280-016-0861-y

M3 - Journal article

C2 - 28116691

AN - SCOPUS:85010383552

VL - 46

SP - 3

EP - 11

JO - Ambio

JF - Ambio

SN - 0044-7447

IS - Suppl. 1

ER -

ID: 173282556