Page 11 - 《高原气象》2025年第5期
P. 11
5 期 张 功等:极地冰区海-气湍流热量交换的研究综述 1129
Duynkerke P G, Roode S T, 2001. Surface energy balance and turbu‐ DOI: 10. 1175/1520-0442(1998)011<0313: TVOTEB>2. 0.
lence characteristics observed at the SHEBA ice camp during CO; 2.
FIRE Ⅲ[J]. Journal of Geophysical Research: Atmospheres, 106 Lique C, Steele M, 2013. Seasonal to decadal variability of Arctic
(D4): 15313-15322. DOI: 10. 1029/2000JD900537. ocean heat content: a model-based analysis and implications for au‐
Elvidge A D, Renfrew I A, Edwards J M, et al, 2023. Improved simu‐ tonomous observing systems[J]. Journal of Geophysical Re‐
lation of the polar atmospheric boundary layer by accounting for search: Oceans, 118(4): 1673-1695. DOI: 10. 1002/jgrc. 20127.
aerodynamic roughness in the parameterization of surface scalar Loose B, Kelly R P, Williams W, et al, 2017. How well does wind
exchange over sea ice[J]. Journal of Advances in Modeling Earth speed predict air-sea gas transfer in the sea ice zone?A synthesis
Systems, 15(3): e2022MS003305. DOI: 10. 1029/2022MS00 of radon deficit profiles in the upper water column of the Arctic
3305. Ocean[J]. Journal of Geophysical Research: Oceans, 122(5):
England M R, Polvani L M, Sun L T, et al, 2020. Tropical climate re‐ 3696-3714. DOI: 10. 1002/2016JC012460.
sponses to projected Arctic and Antarctic sea-ice loss[J]. Nature Lu Y X, Zhou M Y, Wu T W, 2013. Validation of parameterizations
Geoscience, 13(4): 275-281. DOI: 10. 1038/s41561-020- for the surface turbulent fluxes over sea ice with CHINARE 2010
0546-9. and SHEBA data[J]. Polar Research, 32(10): 291-294. DOI:
Fairall C W, Markson R, 1987. Mesoscale variations in surface 10. 3402/polar. v32i0. 20818.
stress, heat fluxes, and drag coefficient in the marginal ice zone Lüpkes C, Gryanik V M, 2015. A stability-dependent parametrization
during the 1983 marginal ice zone experiment[J]. Journal of Geo‐ of transfer coefficients for momentum and heat over polar sea ice to
physical Research: Oceans, 92(C7): 6921-6932. DOI: 10. be used in climate models[J]. Journal of Geophysical Research:
1029/JC092iC07p06921. Atmospheres, 120(2): 552-581. DOI: 10. 1002/2014JD022418.
Fairall C W, Bradley E F, Rogers D P, et al, 1996. Bulk parameter‐ Marcq S, Weiss J, 2012. Influence of sea ice lead-width distribution
ization of air-sea fluxes for tropical ocean-global atmosphere cou‐ on turbulent heat transfer between the ocean and the atmosphere
pled-ocean atmosphere response experiment[J]. Journal of Geo‐ [J]. The Cryosphere, 6(1): 143-156. DOI: 10. 5194/tc-6-143-
physical Research, 101(C2): 3747-3767. DOI: 10. 1029/ 2012.
95JC03205. Martin T, Steele M, Zhang J L, 2014. Seasonality and long-term
Frickenhaus S, Ransby D, Shupe M, et al, 2022. Data from the MO‐ trend of Arctic Ocean surface stress in a model[J]. Journal of
SAiC Arctic Ocean drift experiment[J]. Scientific Data, 9: 568. Geophysical Research: Oceans, 119(3): 1723-1738. DOI: 10.
DOI: 10. 1038/s41597-022-01678-8. 1002/2013JC009425.
Grachev A A, Andreas E L, Fairall C W, et al, 2008. Turbulent mea‐ Massom R A, Harris P T, Michael K J, et al, 1998. The distribution
surements in the stable atmospheric boundary layer during SHE‐ and formative processes of latent-heat polynyas in East Antarctica
BA: ten years after[J]. Acta Geophysica, 56: 142-166. DOI: [J]. Annals of Glaciology, 27: 420-426. DOI: 10. 3189/
10. 2478/s11600-007-0048-9. 1998AoG27-1-420-426.
Gulev S K, Belyaev K P, 2012. Probability distribution characteristics Massom R A, Scambos T A, Bennetts L G, et al, 2018. Antarctic ice
for surface air-sea turbulent heat fluxes over the global ocean[J]. shelf disintegration triggered by sea ice loss and ocean swell[J].
Journal of Climate, 25(1): 184-206. DOI: 10. 1175/2011JCLI4 Nature, 558(7710): 383-389. DOI: 10. 1038/s41586-018-
211. 1. 0212-1.
Inoue J, Hori M E, Enomoto T, et al, 2011. Intercomparison of sur‐ McPhee M G, Ackley S F, Guest P, et al, 1996. The Antarctic zone
face heat transfer near the Arctic marginal ice zone for multiple re‐ flux experiment[J]. Bulletin of the American Meteorological So‐
analyses: a case study of September 2009[J]. Sola, 7: 57-60. ciety, 77(6): 1221-1232. DOI: 10. 1175/1520-0477(1996)077
DOI: 10. 2151/sola. 2011-015. <1221: TAZFE>2. 0. CO; 2.
Jordan R E, Andreas E L, Makshtas A P, 1999. Heat budget of snow- Miller N B, Shupe M D, Cox C J, et al, 2017. Surface energy budget
cover sea ice at North Pole 4[J]. Journal of Geophysical Research: responses to radiative forcing at Summit, Greenland[J]. The
Oceans, 104(C4): 7785-7806. DOI: 10. 1029/1999JC900011. Cryosphere, 11(1): 497-516. DOI: 10. 5194/tc-11-497-2017.
Landy J, Ehn J, Shields M, et al, 2014. Surface and melt pond evolu‐ Overland J E, Dethloff K, Francis J A, et al, 2016. Nonlinear re‐
tion on landfast first-year sea ice in the Canadian Arctic Archipela‐ sponse of mid-latitude weather to the changing Arctic[J]. Nature
go[J]. Journal of Geophysical Research: Oceans, 119(5): 3054- Climate Change, 6: 992-999. DOI: 10. 1038/nclimate3121.
3075. DOI: 10. 1002/2013JC009617. Overland J E, McNutt S, Groves J, et al, 2000. Regional sensible
Li Y B, Gao Z Q, Li D, et al, 2015. An update of non-iterative solu‐ and radiative heat flux estimates for the winter Arctic during the
tions for surface fluxes under unstable conditions[J]. Boundary- Surface Heat Budget of the Arctic Ocean (SHEBA) experiment
Layer Meteorology, 156(3): 501-511. DOI: 10. 1007/s10546- [J]. Journal of Geophysical Research: Oceans, 105(C6):
015-0032-x. 14093-14102. DOI: 10. 1029/1999JC000010.
Lindsay R W, 1998. Temporal variability of the energy balance of Parkinson C L, 2019. A 40-y record reveals gradual Antarctic sea ice
thick arctic pack ice[J]. Journal of Climate, 11(3): 313-333. increases followed by decreases at rates far exceeding the rates

