[1] SMALL T J, DESZOEKE S P, XIEET S P, et al. Air-sea interaction over ocean fronts and eddies [J]. Dynamics of Atmospheres & Oceans, 2008, 45: 274 − 319.
[2] WARNER T T, LAKHTAKIA M N, DOYLE J D. Marine atmospheric boundary layer circulations forced by Gulf Stream sea surface temperature gradients [J]. Monthly Weather Review, 1990, 118: 309 − 323. doi:  10.1175/1520-0493(1990)118<0309:MABLCF>2.0.CO;2
[3] KUWANO Y A, MINOBE S, XIE S P. Precipitation response to the Gulf Stream in an atmospheric GCM [J]. Journal of Climate, 2010, 23: 3676 − 3698. doi:  10.1175/2010JCLI3261.1
[4] MIYAMA T, NONAKA M, NAKAMURA H, et al. A striking early-summer event of a convective rainband persistent along the warm Kuroshio in the East China Sea [J]. Tellus Series A-dynamic Meteorology & Oceanography, 2012, 64: 1 − 9.
[5] XU H, XU M, XIE S P, et al. Deep atmospheric response to the Spring Kuroshio over the East China Sea [J]. Journal of Climate, 2011, 24: 4959 − 4972. doi:  10.1175/JCLI-D-10-05034.1
[6] TANIMOTO Y, KANENARI T, TOKINAGA H, et al. Sea level pressure minimum along the Kuroshio and its extension [J]. Journal of Climate, 2011, 24: 4419 − 4434. doi:  10.1175/2011JCLI4062.1
[7] SASAKI Y N, MINOBE S, MINOBE T, et al. Influence of the Kuroshio in the East China Sea on the early summer (Baiu) rain [J]. Journal of Climate, 2012, 25: 6627 − 6645. doi:  10.1175/JCLI-D-11-00727.1
[8] SKYLLINGSTAD E D, VICKERS D, MAHRT L, et al. Effects of mesoscale sea-surface temperature fronts on the marine atmospheric boundary layer [J]. Boundary-Layer Meteorology, 2007, 123(2): 219 − 237. doi:  10.1007/s10546-006-9127-8
[9] 张苏平, 王媛, 衣立, 等. 一次层积云发展过程对黑潮延伸体海洋锋强迫的响应研究—观测与机制分析[J]. 大气科学, 2017, 41(2): 4 − 12.
[10] CHELTON D B, SCHLAX M G, FREILICH M H, et al. Satellite measurements reveal persistent small-scale features in ocean winds [J]. Science, 2004, 303(5660): 978 − 983. doi:  10.1126/science.1091901
[11] 李博, 周天军, 林鹏飞, 等. 冬季北太平洋海表面热通量异常和海气相互作用的耦合模式模拟[J]. 气象学报, 2011, 69(1): 52 − 63. doi:  10.11676/qxxb2011.005
[12] 晏红明, 李清泉, 袁媛, 等. 夏季西北太平洋大气环流异常及其与热带印度洋—太平洋海温变化的关系[J]. 地球物理学报, 2013, 56(8): 2542 − 2557.
[13] 李琰, 王庆元, 李欢, 等. 前期热带太平洋、印度洋持续性海温异常事件对菲律宾低层大气环流的影响[J]. 热带海洋学报, 2014, 33(1): 36 − 43. doi:  10.3969/j.issn.1009-5470.2014.01.005
[14] 方珂, 余锦华. 北半球热带中太平洋与印度洋海表温度梯度对夏季西北太平洋热带气旋生成频数变化的影响[J]. 热带海洋学报, 2019, 38(5): 42 − 51.
[15] SU F G, HONG Y, LETTENMAIER D P. Evaluation of TRMM multi-satellite precipitation analysis (TMPA) and its hydrologic prediction in the La Plata Basin [J]. Journal of Hydrometeorology, 2008, 9(4): 622 − 640. doi:  10.1175/2007JHM944.1
[16] 白爱娟, 刘长海, 刘晓东. TRMM多卫星降水分析资料揭示的青藏高原及其周边地区夏季降水日变化[J]. 地球物理学报, 2008, 51(3): 704 − 714.
[17] 刘俊峰, 陈仁升, 卿文武, 等. 基于TRMM降水数据的山区降水垂直分布特征[J]. 水科学进展, 2011, 22(4): 447 − 454. doi:  10.14042/j.cnki.32.1309.2011.04.001
[18] SKAMAROCK W C, KLEMP J B, DUDHIA J, et al. A description of the advanced research WRF Version 3 [J]. NCAR Tech, 2008(6): 125.
[19] THOMPSON G, RASMUSSEN R M, MANNING K. Explicit forecasts of winter precipitation using an improved bulk microphysics scheme. Part I: description and sensitivity analysis [J]. Monthly Weather Review, 2004, 132: 519 − 542. doi:  10.1175/1520-0493(2004)132<0519:EFOWPU>2.0.CO;2
[20] TIEDTKE M. A comprehensive mass flux scheme for cumulus parameterization in Large-scale Models [J]. Monthly Weather Review, 1989, 117: 1779 − 1800. doi:  10.1175/1520-0493(1989)117<1779:ACMFSF>2.0.CO;2
[21] MAHRT L, VICKERS D, MOORE E. Flow adjustments across sea-surface temperature changes [J]. Boundary-Layer Meteorology, 2003, 111: 553 − 564.
[22] 陈俊昌. 南海北部冬季海面温度实时分布特征的若干解译[J]. 海洋学报, 1983, 5(3): 391 − 395.
[23] WANG D, LIU Y, QI Y, et al. Seasonal variability of thermal fronts in the northern South China Sea from satellite data [J]. Geophysical Research Letters, 2001, 28(20): 3963 − 3966. doi:  10.1029/2001GL013306
[24] VECCHI G A, XIE S P, FISCHER A S. Ocean-atmosphere co-variability in the Western Arabian Sea [J]. Journal of Climate, 2003, 17: 1213 − 1223.