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Chunming Dong, Hongtao Nie, Xiaofan Luo, Hao Wei, Wei Zhao. Mechanisms for the Link between Onset and Duration of Open Water in the Kara Sea[J]. Acta Oceanologica Sinica. doi: 10.1007/s13131-021-1767-5
Citation: Chunming Dong, Hongtao Nie, Xiaofan Luo, Hao Wei, Wei Zhao. Mechanisms for the Link between Onset and Duration of Open Water in the Kara Sea[J]. Acta Oceanologica Sinica. doi: 10.1007/s13131-021-1767-5

Mechanisms for the Link between Onset and Duration of Open Water in the Kara Sea

doi: 10.1007/s13131-021-1767-5
Funds:  The National Key Research and Development Program of China under contract No. 2016YFC1401401; National Natural Science Foundation of China under contract Nos 41630969, 41941013 and 41806225.
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  • Corresponding author: E-mail: htnie@tju.edu.cn
  • Received Date: 2020-10-27
  • Accepted Date: 2020-11-28
  • Available Online: 2021-04-22
  • The sea ice conditions in the Kara Sea have important impacts on Arctic shipping, oil and gas production, and marine environmental changes. In this study, sea ice coverage (CR) less than 30% is considered as open water, its onset and end dates are defined as Topen and Tclose, respectively. The sea ice melt onset (Tmelt) is defined as the date when ice-sea freshwater flux initially changes from ice into the ocean. Satellite-based sea ice concentration (SIC) from 1989 to 2019 shows a negative correlation between Topen and Tclose (r = –0.77, p < 0.01) in the Kara Sea. This phenomenon is also obtained through analyzing the hindcast simulation from 1994 to 2015 by a coupled ocean and sea-ice model (NAPA1/4). The model results reveal that thermodynamics dominate the sea ice variations, and ice basal melt is greater than the ice surface melt. Heat budget estimation suggests that the heat flux is significant correlated with Topen (r = –0.95, p < 0.01) during the melt period (the duration of multi-year averaged Tmelt to Topen) influenced by the sea ice conditions. Additionally, this heat flux is also suggested to dominate the interannual variation of the heat input during the whole heat absorption process (r = 0.81, p < 0.01). The more heat input during this process leads to later Tclose (r = 0.77, p < 0.01). This is the physical basis of the negative correlation between Topen and Tclose. Therefore, the duration of open water can be predicted by Topen and thence support earlier planning of marine activities.
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  • [1]
    Aksenov Y, Popova E E, Yool A, et al. 2017. On the future navigability of Arctic sea routes: High-resolution projections of the Arctic Ocean and sea ice. Marine Policy, 75: 300–317. doi: 10.1016/j.marpol.2015.12.027
    Barnhart K R, Miller C R, Overeem I, et al. 2016. Mapping the future expansion of Arctic open water. Nature Climate Change, 6(3): 280–285. doi: 10.1038/nclimate2848
    Belchansky G I, Douglas D C, Platonov N G. 2004. Duration of the Arctic Sea ice melt season: Regional and interannual variability, 1979–2001. Journal of Climate, 17(1): 67–80. doi: 10.1175/1520-0442(2004)017<0067:DOTASI>2.0.CO;2
    Bird K J, Charpentier R R, Gautier D L, et al. 2008. Circum-arctic resource appraisal: Estimates of Undiscovered Oil and Gas North of the Arctic Circle. USGS Numbered Series 2008–3049. U.S. Geological Survey, 1–4
    Bitz C M, Holland M M, Weaver A J, et al. 2001. Simulating the ice-thickness distribution in a coupled climate model. Journal of Geophysical Research: Oceans, 106(C2): 2441–2463. doi: 10.1029/1999jc000113
    Blanchard-Wrigglesworth E, Armour K C, Bitz C M, et al. 2011. Persistence and inherent predictability of arctic sea ice in a GCM ensemble and observations. Journal of Climate, 24(1): 231–250. doi: 10.1175/2010JCLI3775.1
    Bliss A C, Anderson M R. 2014. Daily area of snow melt onset on Arctic sea ice from passive microwave satellite observations 1979–2012. Remote Sensing, 6(11): 11283–11314. doi: 10.3390/rs61111283
    Cavalieri D J, Gloersen P, Campbell W J. 1984. Determination of sea ice parameters with the Nimbus 7 SMMR. Journal of Geophysical Research: Atmospheres, 89(D4): 5355–5369. doi: 10.1029/JD089iD04p05355
    Cavalieri D J, Parkinson C L. 2012. Arctic sea ice variability and trends, 1979–2010. The Cryosphere, 6(4): 881–889. doi: 10.5194/tc-6-881-2012
    Chen Ping, Zhao Jinping. 2017. Impacts of surface wind on regional and integrated changes of sea ice in the Arctic. Periodical of Ocean University of China (in Chinese), 47(8): 1–12. doi: 10.16441/j.cnki.hdxb.20160212
    Comiso J C. 1986. Characteristics of Arctic winter sea ice from satellite multispectral microwave observations. Journal of Geophysical Research: Oceans, 91(C1): 975–994. doi: 10.1029/JC091iC01p00975
    Comiso J C, Nishio F. 2008. Trends in the sea ice cover using enhanced and compatible AMSR-E, SSM/I, and SMMR data. Journal of Geophysical Research: Oceans, 113(2): C02S07. doi: 10.1029/2007JC004257
    Curry J A, Schramm J L, Ebert E E. 1995. Sea ice-albedo climate feedback mechanism. Journal of Climate, 8(2): 240–247. doi: 10.1175/1520-0442(1995)008<0240:SIACFM>2.0.CO;2
    Dmitrenko I A, Rudels B, Kirillov S A, et al. 2015. Atlantic water flow into the Arctic Ocean through the St. Anna Trough in the northern Kara Sea. Journal of Geophysical Research: Oceans, 120(7): 5158–5178. doi: 10.1002/2015JC010804
    Duan Chenglin, Dong Sheng, Wang Zhifeng. 2019a. Sea ice regime in the Kara Sea during 2003–2017 based on high-resolution satellite data. Polish Polar Research, 40(3): 205–225. doi: 10.24425/ppr.2019.129671
    Duan Chenglin, Dong Sheng, Xie Zexiao, et al. 2019b. Temporal variability and trends of sea ice in the Kara Sea and their relationship with atmospheric factors. Polar Science, 20: 136–147. doi: 10.1016/j.polar.2019.03.002
    Flanner M G, Shell K M, Barlage M, et al. 2011. Radiative forcing and albedo feedback from the Northern Hemisphere cryosphere between 1979 and 2008. Nature Geoscience, 4(3): 151–155. doi: 10.1038/ngeo1062
    Gautier D L, Bird K J, Charpentier R R, et al. 2009. Assessment of Undiscovered Oil and Gas in the Arctic. Science, 324(5931): 1175–1179. doi: 10.1126/science.1169467
    Hu Xianmin, Sun Jiangfan, Chan T O, et al. 2018. Thermodynamic and dynamic ice thickness contributions in the Canadian Arctic Archipelago in NEMO-LIM2 numerical simulations. The Cryosphere, 12(4): 1233–1247. doi: 10.5194/tc-12-1233-2018
    Ikeda M, Wang Jiang, Zhao Jinping. 2011. Hypersensitive decadal oscillations in the Arctic/subarctic climate. Geophysical Research Letters, 28(7): 1275–1278. doi: 10.1029/2000GL011773
    Johnson M A, Eicken H. 2016. Estimating Arctic sea-ice freeze-up and break-up from the satellite record: A comparison of different approaches in the Chukchi and Beaufort Seas. Elementa-Science of the Anthropocene, 4: 000124. doi: 10.12952/journal.elementa.000124
    Kern S, Harms I, Bakan S, et al. 2005. A comprehensive view of Kara Sea polynya dynamics, sea-ice compactness and export from model and remote sensing data. Geophysical Research Letters, 32(15): L15501. doi: 10.1029/2005GL023532
    Kim K Y, Hamlington B D, Na H N, et al. 2016. Mechanism of seasonal Arctic sea ice evolution and Arctic amplification. The Cryosphere, 10(5): 2191–2202. doi: 10.5194/tc-10-2191-2016
    Lebrun M, Vancoppenolle M, Madec G, et al. 2019. Arctic sea-ice-free season projected to extend into autumn. The Cryosphere, 13(1): 79–96. doi: 10.5194/tc-13-79-2019
    Lei Ruibo, Tian-Kunze X, Leppäranta M, et al. 2016. Changes in summer sea ice, albedo, and portioning of surface solar radiation in the Pacific sector of Arctic Ocean during 1982–2009. Journal of Geophysical Research: Oceans, 121(8): 5470–5486. doi: 10.1002/2016JC011831
    Lei Ruibo, Xie Hongjie, Wang Jia, et al. 2015. Changes in sea ice conditions along the Arctic Northeast Passage from 1979 to 2012. Cold Regions Science and Technology, 119: 132–144. doi: 10.1016/j.coldregions.2015.08.004
    Leifer I, Chen F R, McClimans T, et al. 2018. Satellite ice extent, sea surface temperature, and atmospheric methane trends in the Barents and Kara seas. The Cryosphere Discuss, 1–45. doi: 10.5194/tc-2018-75
    Lien V S, Schlichtholz P, Skagseth Ø, et al. 2017. Wind-driven atlantic water flow as a direct mode for reduced barents sea ice cover. Journal of Climate, 30(2): 803–812. doi: 10.1175/jcli-d-16-0025.1
    Lindsay R, Schweiger A. 2015. Arctic sea ice thickness loss determined using subsurface, aircraft, and satellite observations. The Cryosphere, 9(1): 269–283. doi: 10.5194/tc-9-269-2015
    Lindsay R W, Zhang Jinlun. 2005. The thinning of Arctic Sea Ice, 1988–2003: have we passed a tipping point?. Journal of Climate, 18(22): 4879–4894. doi: 10.1175/JCLI3587.1
    Luo Xiaofan, Hu Xianmin, Nie Hongtao, et al. 2019. Evaluation of hindcast simulation with the ocean and sea-ice model covering the Arctic and adjacent oceans. Haiyang Xuebao (in Chinese), 41(9): 1–12. doi: 10.3969/j.issn.0253-4193.2019.09.001
    Madec, G. 2008. NEMO ocean engine, version 3.6. Note du Pôle de Modélisation, Institut Pierre-Simon Laplace. 27, 386 pp
    Madec G, Imbard M. 1996. A global ocean mesh to overcome the North Pole singularity. Climate Dynamics, 12(6): 381–388. doi: 10.1007/BF00211684
    Markus T, Stroeve J C, Miller J. 2009. Recent changes in Arctic sea ice melt onset, freezeup, and melt season length. Journal of Geophysical Research: Oceans, 114(C12): C12024. doi: 10.1029/2009JC005436
    Maslanik J A, Serreze M C, Barry R G. 1996. Recent decreases in Arctic summer ice cover and linkages to atmospheric circulation anomalies. Geophysical Research Letters, 23(13): 1677–1680. doi: 10.1029/96GL01426
    Meier W N, Fetterer F, Duerr R, et al. 2017. NOAA/NSIDC climate data record of passive microwave sea ice concentration, Version 3. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center, doi: 10.7265/N59P2ZTG
    Mysak L A, Venegas S A. 1998. Decadal climate oscillations in the Arctic: A new feedback loop for atmosphere-ice-ocean interactions. Geophysical Research Letters, 25(19): 3607–3610. doi: 10.1029/98GL02782
    Navy’s Task Force Climate Change. 2014. The United States navy arctic roadmap for 2014 to 2030. Washington, D. C.: University of North Texas Libraries, UNT Digital Library
    Ogi M, Rigor I G, McPhee M G, et al. 2008. Summer retreat of Arctic sea ice: Role of summer winds. Geophysical Research Letters, 35(24): L24701. doi: 10.1029/2008GL035672
    Onarheim I H, Eldevik T, Smedsrud L H, et al. 2018. Seasonal and regional manifestation of arctic sea ice loss. Journal of Climate, 31(12): 4917–4932. doi: 10.1175/JCLI-D-17-0427.1
    Osadchiev A A, Izhitskiy A S, Zavialov P O, et al. 2017. Structure of the buoyant plume formed by Ob and Yenisei river discharge in the southern part of the Kara Sea during summer and autumn. Journal of Geophysical Research: Oceans, 122(7): 5916–5935. doi: 10.1002/2016JC012603
    Perovich D K, Light B, Eicken H, et al. 2007b. Increasing solar heating of the Arctic Ocean and adjacent seas, 1979–2005: Attribution and role in the ice-albedo feedback. Geophysical Research Letters, 34(19): L19505. doi: 10.1029/2007GL031480
    Perovich D K, Nghiem S V, Markus T, et al. 2007a. Seasonal evolution and interannual variability of the local solar energy absorbed by the Arctic sea ice-ocean system. Journal of Geophysical Research: Oceans, 112(3): C03005. doi: 10.1029/2006JC003558
    Polyakov I V, Alekseev G V, Bekryaev R V, et al. 2003. Long-term ice variability in Arctic marginal seas. Journal of Climate, 16(12): 2078–2085. doi: 10.1175/1520-0442(2003)016<2078:LIVIAM>2.0.CO;2
    Rigor I G, Wallace J M, Colony R L. 2002. Response of sea ice to the Arctic oscillation. Journal of Climate, 15(18): 2648–2663. doi: 10.1175/1520-0442(2002)015<2648:ROSITT>2.0.CO;2
    Rousset C, Vancoppenolle M, Madec G, et al. 2015. The Louvain-La-Neuve sea ice model LIM3.6: global and regional capabilities. Geoscientific Model Development, 8(10): 2991–3005. doi: 10.5194/gmd-8-2991-2015
    Screen J A, Simmonds I. 2010. The central role of diminishing sea ice in recent Arctic temperature amplification. Nature, 464(7293): 1334–1337. doi: 10.1038/nature09051
    Serreze M C, Barry R G. 2011. Processes and impacts of Arctic amplification: A research synthesis. Global and Planetary Change, 77(1–2): 85–96. doi: 10.1016/j.gloplacha.2011.03.004
    Serreze M C, Crawford A D, Stroeve J C, et al. 2016. Variability, trends, and predictability of seasonal sea ice retreat and advance in the Chukchi Sea. Journal of Geophysical Research: Oceans, 121(10): 7308–7325. doi: 10.1002/2016JC011977
    Simmonds I. 2015. Comparing and contrasting the behaviour of Arctic and Antarctic sea ice over the 35 year period 1979–2013. Annals of Glaciology, 56(691): 18–28. doi: 10.3189/2015AoG69A909
    Stammerjohn S, Massom R, Rind D, et al. 2012. Regions of rapid sea ice change: An inter-hemispheric seasonal comparison. Geophysical Research Letters, 39(6): L06501. doi: 10.1029/2012GL050874
    Stroeve J C, Crawford A D, Stammerjohn S. 2016. Using timing of ice retreat to predict timing of fall freeze-up in the Arctic. Geophysical Research Letters, 43(12): 6332–6340. doi: 10.1002/2016GL069314
    Stroeve J C, Markus T, Boisvert L, et al. 2014. Changes in Arctic melt season and implications for sea ice loss. Geophysical Research Letters, 41(4): 1216–1225. doi: 10.1002/2013GL058951
    Stroeve J C, Notz D. 2018. Changing state of Arctic sea ice across all seasons. Environmental Research Letters, 13(10): 3001. doi: 10.1088/1748-9326/aade56
    Uotila P, Iovino D, Vancoppenolle M, et al. 2017. Comparing sea ice, hydrography and circulation between NEMO3.6 LIM3 and LIM2. Geoscientific Model Development, 10(2): 1009–1031. doi: 10.5194/gmd-10-1009-2017
    Vancoppenolle M, Fichefet T, Goosse H, et al. 2009. Simulating the mass balance and salinity of Arctic and Antarctic sea ice. 1. Model description and validation. Ocean Modelling, 27(1–2): 33–53. doi: 10.1016/j.ocemod.2008.10.005
    Wang Yali, Luo Xiaofan, Zhang Yongli, et al. 2019a. Heat budget analysis during the ice-melting season in the Chukchi Sea based on a model simulation. Chinese Science Bulletin (in Chinese), 64(33): 3485–3497. doi: 10.1360/N972019-00322
    Wang Yunhe, Bi Haibo, Huang Haijun, et al. 2019b. Satellite-observed trends in the Arctic sea ice concentration for the period 1979–2016. Journal of Oceanology and Limnology, 37(1): 18–37. doi: 10.1007/s00343-019-7284-0
    Woodgate R A. 2018. Increases in the Pacific inflow to the Arctic from 1990 to 2015, and insights into seasonal trends and driving mechanisms from year-round Bering Strait mooring data. Progress in Oceanography, 160: 124–154. doi: 10.1016/j.pocean.2017.12.007
    Woodgate R A, Stafford K M, Prahl F G. 2015. A synthesis of year-round interdisciplinary mooring measurements in the bering strait (1990–2014) and the RUSALCA Years (2004–2011). Oceanography, 28(3SI): 46–67. doi: 10.5670/oceanog.2015.57
    Zhang Jinlun, Rothrock D, Steele M. 2000. Recent changes in Arctic sea ice: The interplay between ice dynamics and thermodynamics. Journal of Climate, 13(17): 3099–3114. doi: 10.1175/1520-0442(2000)013<3099:RCIASI>2.0.CO;2
    Zhang Yongli, Wei Hao, Lu Youyu, et al. 2020. Dependence of Beaufort Sea low ice condition in the summer of 1998 on ice export in the prior winter. Journal of Climate, 33(21): 9247–9259. doi: 10.1175/jcli-d-19-0943.1
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