Spatiotemporal characteristics of sea ice transport in the Baffin Bay and its association with atmospheric variability

Weifu Sun; Haibo Bi; Min Fu; Xi Liang; Yunhe Wang; Yu Liang; Jue Huang; Haijun Huang; Liwen Yan; Qinglong Yu; Shuang Liang

doi:10.1007/s13131-021-1720-7

Volume 40 Issue 3

Apr. 2021

Turn off MathJax

Article Contents

Article Navigation > Acta Oceanologica Sinica > 2021 > 40(3): 1-17

Weifu Sun, Haibo Bi, Min Fu, Xi Liang, Yunhe Wang, Yu Liang, Jue Huang, Haijun Huang, Liwen Yan, Qinglong Yu, Shuang Liang. Spatiotemporal characteristics of sea ice transport in the Baffin Bay and its association with atmospheric variability[J]. Acta Oceanologica Sinica, 2021, 40(3): 1-17. doi: 10.1007/s13131-021-1720-7

Citation:

Weifu Sun, Haibo Bi, Min Fu, Xi Liang, Yunhe Wang, Yu Liang, Jue Huang, Haijun Huang, Liwen Yan, Qinglong Yu, Shuang Liang. Spatiotemporal characteristics of sea ice transport in the Baffin Bay and its association with atmospheric variability[J]. Acta Oceanologica Sinica, 2021, 40(3): 1-17. doi: 10.1007/s13131-021-1720-7

Citation:

Weifu Sun, Haibo Bi, Min Fu, Xi Liang, Yunhe Wang, Yu Liang, Jue Huang, Haijun Huang, Liwen Yan, Qinglong Yu, Shuang Liang. Spatiotemporal characteristics of sea ice transport in the Baffin Bay and its association with atmospheric variability[J]. Acta Oceanologica Sinica, 2021, 40(3): 1-17. doi: 10.1007/s13131-021-1720-7

PDF( 19465 KB)

Spatiotemporal characteristics of sea ice transport in the Baffin Bay and its association with atmospheric variability

doi: 10.1007/s13131-021-1720-7

Weifu Sun¹,
Haibo Bi^{2, 3
,
,},
Min Fu⁴,
Xi Liang⁴,
Yunhe Wang^{3
,
,},
Yu Liang^{3, 5
,},
Jue Huang⁷,
Haijun Huang^{3, 5},
Liwen Yan^{3, 5},
Qinglong Yu⁴,
Shuang Liang⁶

1.
Oceanic Telemetry Engineering and Technology Innovation Center, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
2.
Laboratory for Marine Geology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266037, China
3.
Center for Ocean Mega-Science & Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
4.
National Marine Environmental Forecasting Center, Beijing 100081, China
5.
University of Chinese Academy of Sciences, Beijing 100049, China
6.
Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China
7.
College of Geodesy and Geomatics, Shandong University of Sicence and Technology, Qingdao 266590, China

Funds: The National Key Research and Development Program of China under contract Nos 2016YFA0600102, 2017YFC1405106, 2016YFC1402707, and 2019YFE0114800; the General Project of Natural Science Foundation of Shandong Province under contract No. ZR2020MD100; the Key Deployment Project of Centre for Ocean Mega Science, Chinese Academy of Sciences, under contract No. COMS2020Q12; the National Natural Science Foundation of China under contract Nos 42076185 and 41406215; the Open Fund for the Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences under contract No. MGE2020KG04; the Key R&D Project of Shandong Province under contract No. 2019GSF111017; the NSFC-Shandong Joint Fund for Marine Science Research Centers under contract No. U1606401.

More Information

Author Bio:
liangyu17@mails.ucas.ac.cn
Corresponding author: E-mail: bhb@qdio.ac.cn; wangyunhe@qdio.ac.cn
Received Date: 2020-05-03
Accepted Date: 2020-07-06

Available Online: 2021-04-30

Publish Date: 2021-04-30

Abstract

Abstract

Sea ice export through the Baffin Bay plays a vital role in modulating the sea ice cover variability in the Labrador Sea. In this study, satellite-derived sea ice products are used to obtain the sea ice area flux (SIAF) through the three passages in the Baffin Bay (referred to as A, B, and C for the north, middle, and south passages, respectively). The spatial variability of the monthly sea ice drift in the Baffin Bay is presented. The interannual variability and trends in SIAF via the three passages are outlined. The connection to several large-scale atmospheric circulation modes is assessed. Over the period of 1988–2015, the average annual (October to the following September) SIAF amounts to 555×10³ km², 642×10³ km², and 551×10³ km² through Passages A, B, and C, respectively. These quantities are less than that observed through the Fram Strait (FS, 707×10³ km²) of the corresponding period. The positive trends in annual SIAF, on the order of 53.1×10³ km²/(10 a) and 43.2×10³ km²/(10 a) (significant at the 95% confidence level), are identified at Passages A and B, respectively. The trend of the south passage (C), however, is slightly negative (–13.3×10³ km²/(10 a), not statistically significant). The positive trends in annual SIAF through the Passages A and B are primarily attributable to the significant increases after 2000. The connection between the Baffin Bay sea ice export and the North Atlantic Oscillation is not significant over the studied period. By contrast, the association with the cross-gate sea level pressure difference is robust in the Baffin Bay (R equals 0.69 to 0.71, depending on the passages considered), but relatively weaker than that over FS (R=0.74).
- sea ice transport,
- Baffin Bay,
- Arctic, sea ice area flux (SIAF)

FullText(HTML)

References(46)

References

[1]	Bi Haibo, Huang Haijun, Fu Min, et al. 2016a. Estimating sea-ice volume flux out of the Laptev Sea using multiple satellite observations. Polar Research, 35(1): 24875. doi: 10.3402/polar.v35.24875
[2]	Bi Haibo, Sun Ke, Zhou Xuan, et al. 2016b. Arctic sea ice area export through the fram strait estimated from satellite-based data: 1988–2012. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 9(7): 3144–3157. doi: 10.1109/JSTARS.2016.2584539
[3]	Bi Haibo, Zhang Zehua, Wang Yunhe, et al. 2019. Baffin Bay sea ice inflow and outflow: 1978–1979 to 2016–2017. The Cryosphere, 13(3): 1025–1042. doi: 10.5194/tc-13-1025-2019
[4]	Cho K, Sasaki N, Shimoda H, et al. 1996. Evaluation and improvement of SSM/I sea ice concentration algorithms for the Sea of Okhotsk. Journal of the Remote Sensing Society of Japan, 16(2): 47–58
[5]	Comiso J C, Gersten R A, Stock L V, et al. 2017a. Positive trend in the Antarctic sea ice cover and associated changes in surface temperature. Journal of Climate, 30(6): 2251–2267. doi: 10.1175/JCLI-D-16-0408.1
[6]	Comiso J C, Hall D K. 2014. Climate trends in the Arctic as observed from space. Wiley Interdisciplinary Reviews: Climate Change, 5(3): 389–409. doi: 10.1002/wcc.277
[7]	Comiso J C, Meier W N, Gersten R. 2017b. Variability and trends in the Arctic Sea ice cover: Results from different techniques. Journal of Geophysical Research, 122(8): 6883–6900
[8]	Cuny J, Rhines P B, Kwok R. 2005. Davis Strait volume, freshwater and heat fluxes. Deep Sea Research Part I: Oceanographic Research Papers, 52(3): 519–542. doi: 10.1016/j.dsr.2004.10.006
[9]	Curry B, Lee C M, Petrie B, et al. 2014. Multiyear volume, liquid freshwater, and sea ice transports through Davis Strait, 2004–10. Journal of Physical Oceanography, 44(4): 1244–1266. doi: 10.1175/JPO-D-13-0177.1
[10]	Drinkwater K. 2009. Comparison of the response of Atlantic cod (Gadus morhua) in the high-latitude regions of the North Atlantic during the warm periods of the 1920s–1960s and the 1990s–2000s. Deep Sea Research Part II: Topical Studies in Oceanography, 56(21–22): 2087–2096
[11]	Goosse H, Fichefet T, Campin J M. 1997. The effects of the water flow through the Canadian Archipelago in a global ice-ocean model. Geophysical Research Letters, 24(12): 1507–1510. doi: 10.1029/97GL01352
[12]	Graham R M, Cohen L, Petty A A, et al. 2017. Increasing frequency and duration of Arctic winter warming events. Geophysical Research Letters, 44(13): 6974–6983. doi: 10.1002/2017GL073395
[13]	Häkkinen S, Cavalieri D J. 2005. Sea ice drift and its relationship to altimetry-derived ocean currents in the Labrador Sea. Geophysical Research Letters, 32(11): L11609. doi: 10.1029/2005GL022682
[14]	Hansen A S, Nielsen T G, Levinsen H, et al. 2003. Impact of changing ice cover on pelagic productivity and food web structure in Disko Bay, West Greenland: A dynamic model approach. Deep Sea Research Part I: Oceanographic Research Papers, 50(1): 171–187. doi: 10.1016/S0967-0637(02)00133-4
[15]	Hurrell J W. 1995. Decadal trends in the north atlantic oscillation: regional temperatures and precipitation. Science, 269(5224): 676–679. doi: 10.1126/science.269.5224.676
[16]	Kalnay E, Kanamitsu M, Kistler R, et al. 1996. The NCEP/NCAR 40-year reanalysis project. Bulletin of the American Meteorological Society, 77(3): 437–472. doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2
[17]	Krumpen T, Gerdes R, Haas C, et al. 2016. Recent summer sea ice thickness surveys in Fram Strait and associated ice volume fluxes. The Cryosphere, 10(2): 523–534. doi: 10.5194/tc-10-523-2016
[18]	Krumpen T, Janout M, Hodges K I, et al. 2013. Variability and trends in Laptev Sea ice outflow between 1992–2011. The Cryosphere, 7(1): 349–363. doi: 10.5194/tc-7-349-2013
[19]	Kvamstø N G, Skeie P, Stephenson D B. 2004. Impact of Labrador sea-ice extent on the North Atlantic oscillation. International Journal of Climatology, 24(5): 603–612. doi: 10.1002/joc.1015
[20]	Kwok R. 2000. Recent changes in Arctic Ocean sea ice motion associated with the North Atlantic Oscillation. Geophysical Research Letters, 27(6): 775–778. doi: 10.1029/1999GL002382
[21]	Kwok R. 2007. Baffin Bay ice drift and export: 2002–2007. Geophysical Research Letters, 34(19): L19501. doi: 10.1029/2007GL031204
[22]	Kwok R. 2009. Outflow of Arctic ocean sea ice into the Greenland and Barents Seas: 1979–2007. Journal of Climate, 22(9): 2438–2457. doi: 10.1175/2008JCLI2819.1
[23]	Kwok R, Cunningham G F, Pang S S. 2004. Fram Strait sea ice outflow. Journal of Geophysical Research: Oceans, 109(C1): C01009. doi: 10.1029/2003JC001785
[24]	Kwok R, Maslowski W, Laxon S W. 2005. On large outflows of Arctic sea ice into the Barents Sea. Geophysical Research Letters, 32(22): L22503
[25]	Kwok R, Pedersen L T, Gudmandsen P, et al. 2010. Large sea ice outflow into the Nares Strait in 2007. Geophysical Research Letters, 37(3): L03502
[26]	Kwok R, Spreen G, Pang S. 2013. Arctic sea ice circulation and drift speed: Decadal trends and ocean currents. Journal of Geophysical Research: Oceans, 118(5): 2408–2425. doi: 10.1002/jgrc.20191
[27]	Melling H, Gratton Y, Ingram G. 2001. Ocean circulation within the North Water polynya of Baffin Bay. Atmosphere-Ocean, 39(3): 301–325. doi: 10.1080/07055900.2001.9649683
[28]	Parkinson C L. 2014. Global sea ice coverage from satellite data: Annual cycle and 35-Yr trends. Journal of Climate, 27(24): 9377–9382. doi: 10.1175/JCLI-D-14-00605.1
[29]	Parkinson C L, Cavalieri D J. 2002. A 21 year record of Arctic sea-ice extents and their regional, seasonal and monthly variability and trends. Annals of Glaciology, 34(1): 441–446
[30]	Peterson I K, Pettipas R. 2013. Trends in air temperature and sea ice in the Atlantic Large Aquatic Basin and adjoining areas. Canadian Technical Report of Hydrography and Ocean Sciences, Dartmouth: Fisheries and Oceans Canada, 290.
[31]	Screen J A, Deser C, Simmonds I. 2012. Local and remote controls on observed Arctic warming. Geophysical Research Letters, 39(10): L10709
[32]	Serreze M C, Barrett A P, Stroeve J C, et al. 2009. The emergence of surface-based Arctic amplification. The Cryosphere, 3(1): 11–19. doi: 10.5194/tc-3-11-2009
[33]	Smedsrud L H, Halvorsen M H, Stroeve J C, et al. 2017. Fram Strait sea ice export variability and September Arctic sea ice extent over the last 80 years. The Cryosphere, 11(1): 65–79. doi: 10.5194/tc-11-65-2017
[34]	Smedsrud L H, Sirevaag A, Kloster K, et al. 2011. Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline. The Cryosphere, 5(4): 821–829. doi: 10.5194/tc-5-821-2011
[35]	Spreen G, Kern S, Stammer D, et al. 2006. Satellite-based estimates of sea-ice volume flux through Fram Strait. Annals of Glaciology, 44(1): 321–328
[36]	Stern H L, Heide-Jørgensen M P. 2003. Trends and variability of sea ice in Baffin Bay and Davis Strait, 1953–2001. Polar Research, 22(1): 11–18
[37]	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
[38]	Stroeve J C, Schroder D, Tsamados M, et al. 2018. Warm winter, thin ice?. The Cryosphere, 12(5): 1791–1809. doi: 10.5194/tc-12-1791-2018
[39]	Sumata H, Lavergne T, Girard-Ardhuin F, et al. 2014. An intercomparison of Arctic ice drift products to deduce uncertainty estimates. Journal of Geophysical Research: Oceans, 119(8): 4887–4921. doi: 10.1002/2013JC009724
[40]	Tilling R L, Ridout A, Shepherd A. 2016. Near-real-time Arctic sea ice thickness and volume from CryoSat-2. The Cryosphere, 10(5): 2003–2012. doi: 10.5194/tc-10-2003-2016
[41]	Tschudi M, Meier W N, Stewart J S, et al. 2019. Polar Pathfinder Daily 25 km EASE-Grid Sea Ice Motion Vectors, Version 4. NASA, Boulder, Colorado, doi: 10.5067/INAWUWO7QH7B.
[42]	Wu Bingyi, Zhang Renhe, D’Arrigo R, et al. 2013. On the relationship between winter sea ice and summer atmospheric circulation over eurasia. Journal of Climate, 26(15): 5523–5536. doi: 10.1175/JCLI-D-12-00524.1
[43]	Yang Qian, Dixon T H, Myers P G, et al. 2016. Recent increases in Arctic freshwater flux affects Labrador Sea convection and Atlantic overturning circulation. Nature Communications, 7: 10525. doi: 10.1038/ncomms10525
[44]	Zhang Zehua, Bi Haibo, Sun Ke, et al. 2017. Arctic sea ice volume export through the Fram Strait from combined satellite and model data: 1979–2012. Acta Oceanologica Sinica, 36(1): 44–55. doi: 10.1007/s13131-017-0992-4
[45]	Zhang Xiangdong, Sorteberg A, Zhang Jing, et al. 2008. Recent radical shifts of atmospheric circulations and rapid changes in Arctic climate system. Geophysical Research Letters, 35(22): L22701. doi: 10.1029/2008GL035607
[46]	Zweng M M, Münchow A. 2006. Warming and freshening of Baffin Bay, 1916–2003. Journal of Geophysical Research: Oceans, 111(C7): C07016. doi: 10.1029/2005JC003093