Cited by 87Arctic and Antarctic ice dynamicsClimate variability and modelsArctic and Russian Policy Studies

Arctic Sea Ice in a 1.5°C Warmer World

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Niederdrenk, Anne Laura, Notz, Dirk·2018·Geophysical Research Letters

Abstract

We examine the seasonal cycle of Arctic sea ice in scenarios with limited future global warming. To do so, we analyze two sets of observational records that cover the observational uncertainty of Arctic sea ice loss per degree of global warming. The observations are combined with 100 simulations of historical and future climate evolution from the Max Planck Institute Earth System Model Grand Ensemble. Based on the high‐sensitivity observations, we find that Arctic September sea ice is lost with low probability ( P ≈ 10%) for global warming of +1.5°C above preindustrial levels and with very high probability ( P > 99%) for global warming of +2°C above preindustrial levels. For the low‐sensitivity observations, September sea ice is extremely unlikely to disappear for +1.5°C warming ( P ≪ 1%) and has low likelihood ( P ≈ 10%) to disappear even for +2°C global warming. For March, both observational records suggest a loss of 15% to 20% of Arctic sea ice area for 1.5°C to 2°C global warming.

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  • In the Arctic, sea-ice extent has been found to be linearly related to global-mean temperature, atmospheric CO2 concentration, and anthropogenic CO2 emissions.

    “In the Arctic the latter has been found to be linearly related to global-mean temperature (e.g.Gregory et al., 2002;Niederdrenk and Notz, 2018), atmospheric CO 2 concentration (e.g.Johannessen, 2008;Notz and Marotzke, 2012) and anthropogenic CO 2 emissions (Zickfeld et al., 2012;Herrington and Zickfeld, 2014;Notz and Stroeve, 2016).”

    From Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records (2019) · cites this paper as Niederdrenk and Notz, 2018

    Section 2.2 reports a linear relationship between global-mean temperature and Arctic sea-ice area in observations and simulations. The citing sentence refers to sea-ice extent, whereas the paper explicitly uses area rather than extent (Section 2.1). This citation is attached to the temperature relationship, not the separate claims about CO₂ concentration or emissions. (LLM, conf=0.86)

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  • Observational uncertainty is the main source of uncertainty for estimating at which level of global warming the Arctic will lose its summer sea-ice cover.

    “Niederdrenk and Notz (2018) found that observational uncertainty is the main source of uncertainty for estimating at which level of global warming the Arctic will lose its summer sea-ice cover.”

    From Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records (2019) · cites this paper as Niederdrenk and Notz (2018)

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Research works printed but not linked: 31

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Cited by

Sorted by citations

Authors
Niederdrenk, A. L., & Notz, D.
Affiliations
Max Planck Institute for Meteorology (DE)
Corresponding author
Niederdrenk, Anne Laura
Venue
Geophysical Research Letters
Published
2018-02-20
Volume
45
Issue
4
Pages
1963-1971
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2790794870
Cited by
87
References
2
Citations by year
2026: 4 · 2025: 6 · 2024: 9 · 2023: 13 · 2022: 13 · 2021: 9 · 2020: 14 · 2019: 10 · 2018: 9
FWCI
5.12
Type
journal article
Language
en
Open access
Locations
  • Geophysical Research Letters (publishedVersion)
  • Max Planck Digital Library (submittedVersion)
  • MPG.PuRe (Max Planck Society) (submittedVersion, other-oa)
Funders
German Ministry for Education and Research
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Arctic and Antarctic ice dynamics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Social Sciences › Sociology and Political Science › Arctic and Russian Policy Studies
Keywords
Arctic sea ice, 1.5 °C warming, 2 °C warming, observational uncertainty, climate model ensembles, climate change scenarios

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