The glaciers in the Arctic are affected greatly by the amplified warming of this region. Work now documents a link between variations in the annual mass balance of Arctic glaciers and changes in tropospheric circulation patterns.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$209.00 per year
only $17.42 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Wouters, B., Gardner, A. S. & Moholdt, G. Front. Earth Sci. 7, 96 (2019).
Sasgen, I. et al. Nat. Clim. Change https://doi.org/10.1038/s41558-021-01275-4 (2022).
Gardner, A. S. et al. Nature 473, 357–360 (2011).
Henderson, G. R. et al. Front. Earth Sci. 9, 549 (2021).
Tapley, B. D. et al. Nat. Clim. Change 9, 358–369 (2019).
Velicogna, I. et al. Geophys. Res. Lett. 47, e2020GL087291 (2020).
Amory, C. et al. Geosci. Model Dev. 14, 3487–3510 (2021).
Noël, B. et al. Cryosphere 12, 811–831 (2018).
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Competing interests
The author declares no competing interests.
Rights and permissions
About this article
Cite this article
Sandberg Sørensen, L. Remote connections in the Arctic. Nat. Clim. Chang. 12, 222–223 (2022). https://doi.org/10.1038/s41558-022-01308-6
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41558-022-01308-6