Consequences of Arctic Warming for European Climate and Extreme Weather
Lead Research Organisation:
UNIVERSITY OF EXETER
Department Name: Mathematics
Abstract
The Arctic region is undergoing dramatic changes, in the atmosphere, ocean, ice and on land. The Arctic lower atmosphere is warming at more than twice the rate of the global average, the Arctic sea ice and Greenland Ice Sheet melt have accelerated in the past 30 years. Notable observed changes in the ocean include the freshening of the Beaufort Gyre, and 'Atlantification' of the Barents Sea and of the Eastern Arctic Ocean. Such profound environmental change is likely to have implications across the globe - it is often said, "What happens in the Arctic doesn't stay in the Arctic". Past work has indicated that Arctic amplification can, in principle, affect European climate and extreme weather, but a clear picture of how and why is currently lacking. The 2019 Intergovernmental Panel on Climate Change (IPCC) Special Report on Oceans and Cryosphere concluded "changes in Arctic sea ice have the potential to influence midlatitude weather, but there is low confidence in the detection of this influence for specific weather types".
ArctiCONNECT brings together experts in climate dynamics, polar and subpolar oceanography, and extreme weather, in order to transform understanding of the effects of accelerating Arctic warming on European climate and extreme weather, through an innovative and integrative program of research bridging theory, models of varying complexity, and observations. It will (i) uncover the atmospheric and oceanic mechanisms of Arctic influence on Europe; (ii) determine the ability of state-of-the-art climate models to simulate realistic Arctic-to-Europe teleconnections; and (iii) quantify and understand the contribution of Arctic warming to projected changes in European weather extremes and to the hazards posed to society.
ArctiCONNECT brings together experts in climate dynamics, polar and subpolar oceanography, and extreme weather, in order to transform understanding of the effects of accelerating Arctic warming on European climate and extreme weather, through an innovative and integrative program of research bridging theory, models of varying complexity, and observations. It will (i) uncover the atmospheric and oceanic mechanisms of Arctic influence on Europe; (ii) determine the ability of state-of-the-art climate models to simulate realistic Arctic-to-Europe teleconnections; and (iii) quantify and understand the contribution of Arctic warming to projected changes in European weather extremes and to the hazards posed to society.
Organisations
Publications
Ayres H
(2022)
The Coupled Atmosphere-Ocean Response to Antarctic Sea Ice Loss
in Journal of Climate
Barton B
(2022)
An Ice-Ocean Model Study of the Mid-2000s Regime Change in the Barents Sea
in Journal of Geophysical Research: Oceans
Blackport R
(2020)
Insignificant effect of Arctic amplification on the amplitude of midlatitude atmospheric waves.
in Science advances
Blackport R
(2021)
Decreasing subseasonal temperature variability in the northern extratropics attributed to human influence
in Nature Geoscience
Blackport R
(2021)
Observed Statistical Connections Overestimate the Causal Effects of Arctic Sea Ice Changes on Midlatitude Winter Climate
in Journal of Climate
Blackport R
(2020)
Weakened evidence for mid-latitude impacts of Arctic warming
in Nature Climate Change
Blackport R
(2022)
Arctic change reduces risk of cold extremes.
in Science (New York, N.Y.)
Cai Z
(2024)
Assessing Arctic wetting: Performances of CMIP6 models and projections of precipitation changes
in Atmospheric Research
Chatterjee S
(2023)
Ocean response to reduced Arctic sea ice in PAMIP simulations.
Cornish S
(2021)
Rise and fall of ice production in the Arctic Ocean's ice factories
Cornish SB
(2022)
Rise and fall of sea ice production in the Arctic Ocean's ice factories.
in Nature communications
Cornish SB
(2023)
Impact of sea ice transport on Beaufort Gyre liquid freshwater content.
in Climate dynamics
Cottrell F
(2024)
Signal-to-noise errors in free-running atmospheric simulations and their dependence on model resolution
in Atmospheric Science Letters
Delhaye S
(2023)
Dominant role of early winter Barents-Kara sea ice extent anomalies in subsequent atmospheric circulation changes in CMIP6 models
in Climate Dynamics
Geen R
(2023)
An Explanation for the Metric Dependence of the Midlatitude Jet-Waviness Change in Response to Polar Warming
in Geophysical Research Letters
Hay S
(2022)
Separating the Influences of Low-Latitude Warming and Sea Ice Loss on Northern Hemisphere Climate Change
in Journal of Climate
Hay S
(2023)
The Effect of Arctic Sea-Ice Loss on Extratropical Cyclones
in Geophysical Research Letters
Karpechko A
(2022)
Northern Hemisphere Stratosphere-Troposphere Circulation Change in CMIP6 Models: 1. Inter-Model Spread and Scenario Sensitivity
in Journal of Geophysical Research: Atmospheres
Lewis N
(2024)
The Response of Surface Temperature Persistence to Arctic Sea-Ice Loss
in Geophysical Research Letters
Liang Y
(2024)
The Weakening of the Stratospheric Polar Vortex and the Subsequent Surface Impacts as Consequences to Arctic Sea Ice Loss
in Journal of Climate
Lo Y
(2023)
Changes in Winter Temperature Extremes From Future Arctic Sea-Ice Loss and Ocean Warming
in Geophysical Research Letters
McCrystall M
(2021)
Arctic Winter Temperature Variations Correlated With ENSO Are Dependent on Coincidental Sea Ice Changes
in Geophysical Research Letters
McCrystall MR
(2021)
New climate models reveal faster and larger increases in Arctic precipitation than previously projected.
in Nature communications
Mudhar R
(2023)
Understanding the Stratospheric Response to Arctic Amplification
Oltmanns M
(2024)
European summer weather linked to North Atlantic freshwater anomalies in preceding years
in Weather and Climate Dynamics
Osborne J
(2020)
The North Atlantic as a Driver of Summer Atmospheric Circulation
in Journal of Climate
Richards A
(2022)
Spatial and Temporal Variability of Atlantic Water in the Arctic From 40 Years of Observations
in Journal of Geophysical Research: Oceans
Screen J
(2021)
An ice-free Arctic: what could it mean for European weather?
in Weather
Screen J
(2022)
Net Equatorward Shift of the Jet Streams When the Contribution From Sea-Ice Loss Is Constrained by Observed Eddy Feedback
in Geophysical Research Letters
Smith DM
(2022)
Robust but weak winter atmospheric circulation response to future Arctic sea ice loss.
in Nature communications
Walsh A
(2022)
Non-Linear Response of the Extratropics to Tropical Climate Variability
in Geophysical Research Letters
Warner J
(2020)
Links Between Barents-Kara Sea Ice and the Extratropical Atmospheric Circulation Explained by Internal Variability and Tropical Forcing
in Geophysical Research Letters
Xu M
(2023)
Important role of stratosphere-troposphere coupling in the Arctic mid-to-upper tropospheric warming in response to sea-ice loss
in npj Climate and Atmospheric Science
| Title | Lagrangian trajectory dataset for AMOC lower limb |
| Description | These Lagrangian trajectory files were generated by TRACMASS, a Lagrangian parcel tracing algorithm, using data from a high-resolution (1/12o) ocean sea-ice hindcast. Two set of experiments were performed to trace the Atlantic Meridional Overturning Circulation (AMOC) lower limb; 1) Initiated only southward trajectories across the Fram Strait (fs) that corresponds to Arctic outflow and 2) traced only northward trajectories across the easten Subpolar North Atlantic (SPNA) Section which corresponds to Atlantic inflow and associated with the North Atlantic Current (nac). _ini.csv = store positions and properties of trajectories at the starting location _run.csv = store positions and properties of trajectories during the trajectory simulation _out.csv = store positions and properties of trajectories at the ending location _rerun.csv = This file is used to select trajectories that have reached a particular ending section. Column 2 in this file contain kill zone flag. Flag 1 means trajectories reaching the surface, 2 indicates trajectories reaching the Fram Strait , 3 means trajectories reaching the eastern SPNA section and finally 4 illustrate trajectories aprroaching the Barents Sea. TRACMASS documentation is available at https://www.tracmass.org/docs.html |
| Type Of Material | Database/Collection of data |
| Year Produced | 2023 |
| Provided To Others? | Yes |
| URL | https://zenodo.org/doi/10.5281/zenodo.7924419 |