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第 50 卷第 9 期        江   萌等:北极海冰区 1981—2020 年辐射通量的时空变化特征与分析                            1925

                    Sea  Ice  from  Satellite  Observations[J].   Remote   tion from MODIS Data Using Principal Components

                    Sensing, 2022, 14(8):1846-1846.                  Regression  Method:  Fars  Province  Case  Study[J].
               [7]  MARKUS  T,  STROEVE  J  C,  MILLER  J.   Re⁃     International Agrophysics, 31(1): 23-34.
                    cent  Changes  in  Arctic  Sea  Ice  Melt  Onset,  Free-  [18]  WANG  X,  LIU  J,  YANG  B  Y,  et  al.   Seasonal
                    zeup, and Melt Season Length[J].  Journal of Geo⁃  Trends in Clouds and Radiation over the Arctic Seas
                    physical  Research:  Oceans,  2009,  114 (C12) :   from  Satellite  Observations  During  1982  to  2019
                    C12024.                                         [J].  Remote Sensing, 2021, 13(16): 3201.
               [8]  STROEVE J C, MARKUS T, BOISVERT L, et       [19]  RAMANATHAN  V,  CESS  R  D,  HARRISON  E
                    al.   Changes  in  Arctic  Melt  Season  and  Implications   F, et al.  Cloud-Radiative Forcing and Climate: Re⁃
                    for Sea Ice Loss[J].  Geophysical Research Letters,   sults  from  the  Earth  Radiation  Budget  Experiment
                    2014, 41(4): 1216-1225.                         [J].  Science, 1989, 243(4887): 57-63.
               [9]  PENG H T, KE C Q, SHEN X Y, et al.  Summer   [20]  RAMANATHAN  V,  SUBASILAR  B,  ZHANG
                    Albedo Variations in the Arctic Sea Ice Region from   G J, et al.  Warm Pool Heat Budget and Shortwave
                    1982 to 2015[J].  International Journal of Climato⁃  Cloud  Forcing:  A  Missing  Physics[J].   Science,
                    logy, 2020, 40(6): 3008-3020.                    1995, 267(5197): 499-503.
               [10]  NICOLAUS M, KATLEIN C, MASLANIK J, et      [21]  SHUPE  M  D,  INTRIERI  J  M.   Cloud  Radiative
                    al.   Changes  in  Arctic  Sea  Ice  Result  in  Increasing   Forcing  of  the  Arctic  Surface:  The  Influence  of
                    Light  Transmittance  and  Absorption[J].   Geophysi⁃  Cloud Properties, Surface Albedo, and Solar Zenith
                    cal Research Letters, 2012, 39(24): L24501.      Angle[J].   Journal  of  Climate,  2004,  17(3):
               [11]  WANG C X, GRANSKOG M A, HUDSON S R,             616-628.
                    et  al.   Atmospheric  Conditions  in  the  Central  Arctic   [22]  ALKAMA  R,  TAYLOR  P  C,  GARCIA-SAN
                    Ocean Through the Melt Seasons of 2012 and 2013:   MARTIN L, et al.  Clouds Damp the Radiative Im⁃
                    Impact on Surface Conditions and Solar Energy De⁃  pacts  of  Polar  Sea  Ice  Loss[J].   The  Cryosphere,
                    position  into  the  Ice-Ocean  System[J].   Journal  of   2020, 14(8): 2673-2686.
                    Geophysical  Research:  Atmospheres,  2016,  121  [23]  CHERNOKULSKY A, MOKHOV I I.  Climatolo⁃
                    (3): 1043-1058.                                  gy  of  Total  Cloudiness  in  the  Arctic:  An  Intercom⁃
               [12]  CHOI Y S, HWANG J, OK J, et al.  Effect of Arc⁃  parison of Observations and Reanalyses[J].  Advances
                    tic  Clouds  on  the  Ice-Albedo  Feedback  in  Midsum⁃  in Meteorology, 2012, 2012(1): 542093.
                    mer [J].   International  Journal  of  Climatology,   [24]  TSAY S C, STAMNES K, JAYAWEERA K.  Ra⁃
                    2020, 40(10): 4707-4714.                         diative Energy Budget in the Cloudy and Hazy Arctic
               [13]  ZHANG  T,  ZHOU  C  X,  ZHENG  L.   Analysis  of   [J].  Journal of the Atmospheric Sciences, 1989, 46
                    the  Temporal-Spatial  Changes  in  Surface  Radiation   (7): 1002-1018.
                    Budget over the Antarctic Sea Ice Region[J].  Science   [25]  INTRIERI  J  M,  FAIRALL  C  W,  SHUPE  M  D,
                    of the Total Environment, 2019, 666: 1134-1150.  et  al.   An  Annual  Cycle  of  Arctic  Surface  Cloud
               [14]  SEDLAR  J,  TJERNSTRÖM  M,  MAURITSEN           Forcing at SHEBA[J].  Journal of Geophysical Re⁃
                    T,  et  al.   A  Transitioning  Arctic  Surface  Energy   search:  Oceans,  2002,  107(C10) :  SHE13-1-
                    Budget:  The  Impacts  of  Solar  Zenith  Angle,  Sur⁃  SHE13-14.
                    face  Albedo  and  Cloud  Radiative  Forcing[J].   Cli⁃  [26]  EBELL  K,  NOMOKONOVA  T,  MATURILLI

                    mate Dynamics, 2011, 37(7): 1643-1660.           M,  et  al.   Radiative  Effect  of  Clouds  at  Ny-Ale⁃
               [15]  KAPSCH  M  L,  GRAVERSEN  R  G,  TJERN⁃         sund, Svalbard, as Inferred from Ground-Based Re⁃
                    STRÖM  M,  et  al.   The  Effect  of  Downwelling   mote  Sensing  Observations[J].   Journal  of  Applied
                    Longwave and Shortwave Radiation on Arctic Sum⁃  Meteorology and Climatology, 2022, 59(1): 3-22.
                    mer Sea Ice[J].  Journal of Climate, 2016, 29(3):   [27]  DONG  X  Q,  XI  B  K,  CROSBY  K,  et  al.   A  10
                    1143-1159.                                       Year  Climatology  of  Arctic  Cloud  Fraction  and  Ra⁃
               [16]  MORTIN  J,  SVENSSON  G,  GRAVERSEN  R          diative  Forcing  at  Barrow,  Alaska[J].   Journal  of
                    G, et al.  Melt Onset over Arctic Sea Ice Controlled   Geophysical  Research:  Atmospheres,  2010,  115
                    by  Atmospheric  Moisture  Transport[J].   Geophysi⁃  (D17): D17212
                    cal Research Letters, 2016, 43(12): 6636-6642.  [28]  HUANG Y Y, DONG X Q, XI B K, et al.  Quanti⁃
               [17]  BARZIN  R,  SHIRVANI  A,  LOTFI  H.   Estima⁃   fying  the  Uncertainties  of  Reanalyzed  Arctic  Cloud
                    tion  of  Daily  Average  Downward  Shortwave  Radia⁃  and Radiation Properties Using Satellite Surface Ob⁃
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