大气边界层物理研究进展

[1] Stochastic modeling the effect of wind gust on dust entrainment during sand storm [J]. CHINESE SCIENCE BULLETIN, 2012, 57 (27): : 3595 - 3602

[2] Simulation of wind gust structure in the atmospheric boundary layer with Lattice Boltzmann Method[J]. CHENG XueLing,HU Fei & ZENG QingCun State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China.Chinese Science Bulletin. 2012(10)

[3] 半干旱区不同下垫面地表粗糙度和湍流通量整体输送系数变化特征 [J]. 中国科学:地球科学, 2012, 42 (01) : 24 - 33

[4] 风能资源评估中地表粗糙度的研究 [J]. 资源科学, 2011, 33 (12) : 2341 - 2348

[5] Analysis of Atmospheric Boundary Layer Height Characteristics over the Arctic Ocean Using the Aircraft and GPS Soundings[J]. DAI Cheng-Ying1, 2, GAO Zhi-Qiu1, WANG Qing3, and CHENG Gang4 1 State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China 3 Naval Postgraduate School, CA 93940, USA 4 Department o

[6] Vertical Air Mass Exchange Driven by the Local Circulation on the Northern Slope of Mount Everest[J]. 周立波,邹捍,马舒坡,李鹏,朱金焕,霍翠萍.Advances in Atmospheric Sciences. 2011(01)

[7] 内蒙古羊草和大针茅草原下垫面水汽、CO通量输送特征 [J]. 高原气象 , 2010, (03) : 605 - 613

[8] 喜马拉雅山地区地气间物质交换及其与南亚夏季风的联系 [J]. 气候与环境研究, 2010, 15 (03) : 289 - 294

[9] Gustiness and Coherent Structure of Strong Winds and Their Role in Dust Emission and Entrainment[J]. 曾庆存,程雪玲,胡非,彭珍.Advances in Atmospheric Sciences. 2010(01)

[10] 放牧强度对内蒙古半干旱草原地气间能量和物质交换的影响 [J]. 大气科学, 2009, 33 (06) : 1201 - 1211

[1] Stochastic modeling the effect of wind gust on dust entrainment during sand storm [J]. CHINESE SCIENCE BULLETIN, 2012, 57 (27): : 3595 - 3602

[2] Simulation of wind gust structure in the atmospheric boundary layer with Lattice Boltzmann Method[J]. CHENG XueLing,HU Fei & ZENG QingCun State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China.Chinese Science Bulletin. 2012(10)

[3] 半干旱区不同下垫面地表粗糙度和湍流通量整体输送系数变化特征 [J]. 中国科学:地球科学, 2012, 42 (01) : 24 - 33

[4] 风能资源评估中地表粗糙度的研究 [J]. 资源科学, 2011, 33 (12) : 2341 - 2348

[5] Analysis of Atmospheric Boundary Layer Height Characteristics over the Arctic Ocean Using the Aircraft and GPS Soundings[J]. DAI Cheng-Ying1, 2, GAO Zhi-Qiu1, WANG Qing3, and CHENG Gang4 1 State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 2 Graduate University of Chinese Academy of Sciences, Beijing 100049, China 3 Naval Postgraduate School, CA 93940, USA 4 Department o

[6] Vertical Air Mass Exchange Driven by the Local Circulation on the Northern Slope of Mount Everest[J]. 周立波,邹捍,马舒坡,李鹏,朱金焕,霍翠萍.Advances in Atmospheric Sciences. 2011(01)

[7] 内蒙古羊草和大针茅草原下垫面水汽、CO通量输送特征 [J]. 高原气象 , 2010, (03) : 605 - 613

[8] 喜马拉雅山地区地气间物质交换及其与南亚夏季风的联系 [J]. 气候与环境研究, 2010, 15 (03) : 289 - 294

[9] Gustiness and Coherent Structure of Strong Winds and Their Role in Dust Emission and Entrainment[J]. 曾庆存,程雪玲,胡非,彭珍.Advances in Atmospheric Sciences. 2010(01)

[10] 放牧强度对内蒙古半干旱草原地气间能量和物质交换的影响 [J]. 大气科学, 2009, 33 (06) : 1201 - 1211