Articles | Volume 19, issue 6
https://doi.org/10.5194/acp-19-3927-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-19-3927-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Heat transport pathways into the Arctic and their connections to surface air temperatures
Leipzig Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Christoph Jacobi
Leipzig Institute for Meteorology, Universität Leipzig, Leipzig, Germany
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Cited
22 citations as recorded by crossref.
- Contrasting extremely warm and long-lasting cold air anomalies in the North Atlantic sector of the Arctic during the HALO-(𝒜 𝒞)3 campaign A. Walbröl et al. 10.5194/acp-24-8007-2024
- Distinct Role of a Spring Atmospheric Circulation Mode in the Arctic Sea Ice Decline in Summer H. Bi et al. 10.1029/2022JD037477
- Surface impacts and associated mechanisms of a moisture intrusion into the Arctic observed in mid-April 2020 during MOSAiC B. Kirbus et al. 10.3389/feart.2023.1147848
- Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps D. Mewes & C. Jacobi 10.3390/atmos11030251
- Projections of an ice-free Arctic Ocean A. Jahn et al. 10.1038/s43017-023-00515-9
- Water vapor satellite products in the European Arctic: An inter-comparison against GNSS data J. Vaquero-Martínez et al. 10.1016/j.scitotenv.2020.140335
- Influence of Regional Warming on Primary Production of the Kara Sea during the Last Two Decades (2002–2021) A. Demidov et al. 10.31857/S0030157423020028
- Airmass Analysis of Size-Resolved Black Carbon Particles Observed in the Arctic Based on Cluster Analysis R. Cremer et al. 10.3390/atmos13050648
- Synoptic controls on warm-season O3 pollution in eastern China: A focus on O3-NOx-VOC chemistry Z. Liao et al. 10.1016/j.atmosres.2024.107660
- The impact of concurrent variation of atmospheric meridional heat transport in western Baffen Bay and eastern Greenland on summer Arctic sea ice L. Wang et al. 10.1007/s13131-020-1614-0
- Impact of Regional Warming on Primary Production of the Kara Sea in the Last Two Decades (2002–2021) A. Demidov et al. 10.1134/S0001437023020029
- Effects of variable ice–ocean surface properties and air mass transformation on the Arctic radiative energy budget M. Wendisch et al. 10.5194/acp-23-9647-2023
- Arctic climate response to European radiative forcing: a deep learning study on circulation pattern changes S. Mehrdad et al. 10.5194/wcd-5-1223-2024
- Investigating Wintertime Cloud Microphysical Properties and Their Relationship to Air Mass Advection at Ny-Ålesund, Svalbard Using the Synergy of a Cloud Radar–Ceilometer–Microwave Radiometer Y. Cho et al. 10.3390/rs13132529
- The 2018 North Greenland polynya observed by a newly introduced merged optical and passive microwave sea-ice concentration dataset V. Ludwig et al. 10.5194/tc-13-2051-2019
- From a polar to a marine environment: has the changing Arctic led to a shift in aerosol light scattering properties? D. Heslin-Rees et al. 10.5194/acp-20-13671-2020
- The influence of water vapor anomalies on clouds and their radiative effect at Ny-Ålesund T. Nomokonova et al. 10.5194/acp-20-5157-2020
- Local and Remote Atmospheric Circulation Drivers of Arctic Change: A Review G. Henderson et al. 10.3389/feart.2021.709896
- Arctic Lower-Tropospheric Warm and Cold Extremes: Horizontal and Vertical Transport, Diabatic Processes, and Linkage to Synoptic Circulation Features L. Papritz 10.1175/JCLI-D-19-0638.1
- Arctic amplification of climate change: a review of underlying mechanisms M. Previdi et al. 10.1088/1748-9326/ac1c29
- Combining low- and high-frequency microwave radiometer measurements from the MOSAiC expedition for enhanced water vapour products A. Walbröl et al. 10.5194/amt-17-6223-2024
- Accelerated decline of summer Arctic sea ice during 1850–2017 and the amplified Arctic warming during the recent decades Q. Cai et al. 10.1088/1748-9326/abdb5f
22 citations as recorded by crossref.
- Contrasting extremely warm and long-lasting cold air anomalies in the North Atlantic sector of the Arctic during the HALO-(𝒜 𝒞)3 campaign A. Walbröl et al. 10.5194/acp-24-8007-2024
- Distinct Role of a Spring Atmospheric Circulation Mode in the Arctic Sea Ice Decline in Summer H. Bi et al. 10.1029/2022JD037477
- Surface impacts and associated mechanisms of a moisture intrusion into the Arctic observed in mid-April 2020 during MOSAiC B. Kirbus et al. 10.3389/feart.2023.1147848
- Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps D. Mewes & C. Jacobi 10.3390/atmos11030251
- Projections of an ice-free Arctic Ocean A. Jahn et al. 10.1038/s43017-023-00515-9
- Water vapor satellite products in the European Arctic: An inter-comparison against GNSS data J. Vaquero-Martínez et al. 10.1016/j.scitotenv.2020.140335
- Influence of Regional Warming on Primary Production of the Kara Sea during the Last Two Decades (2002–2021) A. Demidov et al. 10.31857/S0030157423020028
- Airmass Analysis of Size-Resolved Black Carbon Particles Observed in the Arctic Based on Cluster Analysis R. Cremer et al. 10.3390/atmos13050648
- Synoptic controls on warm-season O3 pollution in eastern China: A focus on O3-NOx-VOC chemistry Z. Liao et al. 10.1016/j.atmosres.2024.107660
- The impact of concurrent variation of atmospheric meridional heat transport in western Baffen Bay and eastern Greenland on summer Arctic sea ice L. Wang et al. 10.1007/s13131-020-1614-0
- Impact of Regional Warming on Primary Production of the Kara Sea in the Last Two Decades (2002–2021) A. Demidov et al. 10.1134/S0001437023020029
- Effects of variable ice–ocean surface properties and air mass transformation on the Arctic radiative energy budget M. Wendisch et al. 10.5194/acp-23-9647-2023
- Arctic climate response to European radiative forcing: a deep learning study on circulation pattern changes S. Mehrdad et al. 10.5194/wcd-5-1223-2024
- Investigating Wintertime Cloud Microphysical Properties and Their Relationship to Air Mass Advection at Ny-Ålesund, Svalbard Using the Synergy of a Cloud Radar–Ceilometer–Microwave Radiometer Y. Cho et al. 10.3390/rs13132529
- The 2018 North Greenland polynya observed by a newly introduced merged optical and passive microwave sea-ice concentration dataset V. Ludwig et al. 10.5194/tc-13-2051-2019
- From a polar to a marine environment: has the changing Arctic led to a shift in aerosol light scattering properties? D. Heslin-Rees et al. 10.5194/acp-20-13671-2020
- The influence of water vapor anomalies on clouds and their radiative effect at Ny-Ålesund T. Nomokonova et al. 10.5194/acp-20-5157-2020
- Local and Remote Atmospheric Circulation Drivers of Arctic Change: A Review G. Henderson et al. 10.3389/feart.2021.709896
- Arctic Lower-Tropospheric Warm and Cold Extremes: Horizontal and Vertical Transport, Diabatic Processes, and Linkage to Synoptic Circulation Features L. Papritz 10.1175/JCLI-D-19-0638.1
- Arctic amplification of climate change: a review of underlying mechanisms M. Previdi et al. 10.1088/1748-9326/ac1c29
- Combining low- and high-frequency microwave radiometer measurements from the MOSAiC expedition for enhanced water vapour products A. Walbröl et al. 10.5194/amt-17-6223-2024
- Accelerated decline of summer Arctic sea ice during 1850–2017 and the amplified Arctic warming during the recent decades Q. Cai et al. 10.1088/1748-9326/abdb5f
Latest update: 01 Nov 2024
Short summary
Horizontal moist static energy (MSE) transport patterns were extracted from reanalysis data using an artificial neuronal network for the winter months. The results show that during the last 30 years transport pathways that favour MSE transport through the North Atlantic are getting more frequent. This North Atlantic pathway is connected to positive temperature anomalies over the central Arctic, which implies a connection between Arctic amplification and the change in horizontal heat transport.
Horizontal moist static energy (MSE) transport patterns were extracted from reanalysis data...
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