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| 1 | Climatic and lake environmental changes in the Serling Co region of Tibet over a variety of timescales显示文摘The Serling Co region is located at the transitional zone of the interaction between the Indian monsoon and the westerlies over the Tibetan Plateau. The Serling Co lake covers a water area of2,389 km2(June 2017) in a 45,530 km2drainage basin. Under the dramatic hydro-meteorological changes on the Tibetan Plateau in recent decades, and complex hydrological compositions of rivers and lakes in the basin, the lake area expanded by 43%, from1,667 km2in 1976, to 2,389 km2in 2017 (1)In 2014 it surpassed Nam Co as the largest lake on the Tibetan Plateau [2], and exerts significant effect on regional environmental conditions. | Liping Zhu Junbo Wang Jianting Ju Ning Ma Yinsheng Zhang Chong Liu Boping Han Linshan Liu Mingda Wang Qingfeng Ma | 2019 | Science Bulletin2019，64，7： | 13 |
| 2 | A three-dimensional coupled physical-biological model study in the spring of 1993 in the Bohai Sea of China显示文摘A three-dimensional (3-D) coupled physical and biological model was used to investigate the physical processes and their influence on the ecosystem dynamics of the Bohai Sea of China. The physical processes include M2 tide, time-varying wind forcing and river discharge. Wind records from 1 to 31 May in 1993 were selected to force the model. The biological model is based on a simple, nitrate and phosphate limited, lower trophic food web system. The simulated results showed that variation of residual currents forced by M2 tide, river discharge and time-varying wind had great impact on the distribution of phytoplankton biomass in the Laizhou Bay. High phytoplankton biomass appeared in the upwelling region. Numerical experiments based on the barotropic model and baroclinic model with no wind and water discharge were also conducted. Differences in the results by the baroclinic model and the barotropic model were significant: more patches appeared in the baroclinic model comparing with the barotropic model. And in the baroclinic model, the subsurface maximum phytoplankton biomass patches formed in the stratified water. | WANG Hui LIU Guimei SUN Song HAN Boping FU Xiang | 2007 | Acta Oceanologica Sinica2007，26，6： | 3 |
| 3 | Preface: conservation, management, and restoration of shallow lake ecosystems facing t multiple stressors显示文摘 | LIU Zhengwen HAN Boping GULATI R D | 2013 | Hydrobiologia2013，710，1： | 1 |
| 4 | The thermal structure of San Reservoir (NE: Spain): a simulation approach显示文摘 | HAN Boping ARMENGOL J GARCIA J C | 2000 | Ecological Modelling2000，125，： | 1 |
| 5 | Floating-leavedmacrophyte ( Trapa quadrispinosa Roxb) beds have significanteffects on sediment resuspension in Lake Taihu, China 显示文摘 | HUANG Peisheng HAN Boping LIU Zhengwen | 2007 | Hydrobiologia2007，581，1： | 1 |
| 6 | Analysis of grey model between seawater environmentalessential factors and phytoplankon dynamics in the Dapeng Bay, the South China Sea显示文摘The relation between the dynamics of phytoplankton and essential environmental factors of seawater has been studied. According to the comparison between environmental factors of seawater. and on the basis of mathematical space theory and the four principles of normalization, even symmetry, globality and proximity, smoothing discrete function, the grey derivative and the grey differential equation have been defined, the grey models and relation to the factors (the seawater physical and chemical factors) were estimated. The calculation results indicate that zooplankton,Mn, Fe and dissolved oxygen are the moot important factors. | Huang Weijian Qi Yuzao Han Boping and Chen Shurong | 1999 | Acta Oceanologica Sinica1999，18，1： | 1 |
| 7 | Control mechanisms of Diel Vertical Migration: theoretical assumptions显示文摘 | HAN Boping STRASKRABA Milan | 2001 | Journal of Theoretical Biology2001，210，： | 1 |
| 8 | Estimation of total cloud cover from solar radiation observations at Lake Rotorua, New Zealand显示文摘 | LUO Liancong HAMILTON D HAN Boping | 2010 | Solar Energy2010，84，3： | 1 |
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