青藏高原湖泊水文变化规律、驱动因素及影响反馈:从遥感视角:pattern drivers and impacts9787030753427
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库存17件
作者宋春桥
出版社科学出版社
ISBN9787030753427
出版时间2023-07
装帧精装
开本其他
定价269元
货号17025801
上书时间2024-12-17
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作者简介
2018年,入选江苏省人才项目;2018年,入选江苏省“333人才工程”学术技术带头人;2020年,获教育部科学研究优秀成果奖自然科学二等奖 (3rd);2021年,国家人才项目结题优秀(院)
目录
Contents
Foreword
Preface
Section I Pattern
Chapter 1 Modeling and Analysis of Lake Water Storage Changes on the Tibetan Plateau Using Multi-mission Satellite Data 3
1.1 Research objective 3
1.2 Study area 4
1.3 Materials and methodology 5
1.3.1 ICESat satellite altimetry data 5
1.3.2 Optical satellite images 6
1.3.3 GRACE satellite gravimetry data 6
1.3.4 Monitoring lake water extent changes 7
1.3.5 Modeling lake water storage changes 8
1.4 Water level changes in 30 typical lakes on the TP 10
1.5 Surface area changes in all lakes on the TP 11
1.6 Modeling lake water storage variations on the TP 13
1.7 Mass changes on the TP observed from GRACE satellite gravimetry 18
1.8 Limitations and uncertainty analyses 19
1.9 Summary 20
References 21
Chapter 2 Refined Estimation of Lake Water Level and Storage Changes on the Tibetan Plateau from ICESat/ICESat-2 25
2.1 Research objective 25
2.2 Study lakes on the Tibetan Plateau 26
2.3 Materials and methods 27
2.3.1 ICESat/ICESat-2 data for deriving lake levels from 2003 to 2020 27
2.3.2 Lake area derived from Global Land Analysis and Discovery (GLAD) data 28
2.3.3 Lake mapping and storage variation from 2003 to 2019 28
2.3.4 Classification of the TP lakes as closed and upstream types 29
2.4 Coverage of ICESat/ICESat-2 measurements over the TP lakes 29
2.5 Lake level changes between 2003 and 2020 31
2.6 Lake water storage changes between 2003 and 2020 32
2.7 Uncertainty in estimating lake water storage changes on the TP 33
2.8 Comparison of lake changes during the ICESat era and joint-mission period 34
2.9 Summary 35
References 36
Chapter 3 Heterogeneous Hydrologic Changes of TP Lakes Observed by Multi-mission Altimeters 39
3.1 Research objective 39
3.2 Study lakes on the Tibetan Plateau 40
3.3 Study data and methods 42
3.3.1 CryoSat-2 altimetry data 42
3.3.2 ICESat altimetry data 43
3.3.3 Other sources of radar altimetry data archives 43
3.3.4 In-situ lake level observations and other materials 44
3.3.5 Data processing and estimation of lake level trends 46
3.4 Evaluation of CryoSat-2 altimetry data on the two typical lakes 47
3.5 Heterogeneous changes in water level for the TP lakes based on combined ICESat/CryoSat-2 altimetry data 49
3.6 Heterogeneous water level variations of typical large lakes based on multi-source merged radar altimetry data 52
3.7 Possible cause of the heterogeneous change patterns of the TP lakes 56
3.8 Summary 58
References 59
Chapter 4 Seasonal and Abrupt Changes in Water Level of the Lakes on the Tibetan Plateau 63
4.1 Research objective 63
4.2 Study lakes 64
4.3 Data and methods 64
4.3.1 ICESat altimetry data to extract lake water level data 64
4.3.2 Meteorological data 65
4.3.3 GRACE gravimetric terrestrial water storage data 66
4.3.4 Definition and retrieval of seasonal lake water level variations 67
4.3.5 Cluster analysis onchange patterns of lake level 71
4.3.6 Conceptual model of lake water balances 72
4.4 Comparison of time-series lake level variations during warm and cold seasons 73
4.5 Cluster-based spatial pattern on seasonal and abrupt water level changes 75
4.6 The correlations between abrupt changes in lake level and climatic variables in abnormal years 77
4.7 Comparison of GRACE-observed TWS changes and seasonal and abrupt lake-level variations 80
4.8 Evaluations of cluster-based lake changing patterns 82
4.9 The associations of lake expansions with the precipitation, evaporation and glacial meltwater 83
4.10 Summary 84
References 85
Section II Drivers
Chapter 5 Accelerated Lake Expansion on the Tibetan Plateau in the 2000s: Induced by Glacial Melting or Other Processes? 91
5.1 Research objective 91
5.2 Study area, materials, and methods 92
5.2.1 The TP lakes and climate 92
5.2.2 Optical images for measuring lake area variations 93
5.2.3 Satellite altimetry data for measuring lake water level variations 94
5.2.4 Other materials and data processing 98
5.2.5 Linear model of the water level change rate and the analyzed factors 99
5.3 Comparing the lake variation characteristics in the 2000s and the 1970–2000 99
5.4 Analysis of the relationship between lake changes and the glacier meltwater supply and lake supply coefficient at the plateau scale 102
5.5 Analysis of the interzone difference in the relationship between lake changes and the glacier wastage and supply coefficient 103
5.6 The relationship between lake changes and the precipitation and evapotranspiration variability 106
5.7 Comparative analyses based on typical lake cases 107
5.8 Uncertainty analyses 108
5.9 Summary 110
References 111
Chapter 6 The Climate Cause of Spatio-temporal Heterogeneous Changes in Lake Level on the Tibetan Plateau and Surroundings 115
6.1 Research objective 115
6.2 Study area and materials 116
6.2.1 Study area 116
6.2.2 Data sources 117
6.2.3 Correlation analyses on the lake level variations and climatic variability 124
6.3 Cross-evaluation of lake levels from different altimetry data sets 125
6.4 Heterogeneous change patterns of lake level derived from multiple satellite altimetry data 126
6.5 Correlation analyses on lake level variations and gauge-based climate variables 128
6.6 Relationships of lake area and level changes and basin-wide gridded precipitation variability 130
6.7 Comparison with prior studies 132
6.8 Summary 134
References 135
Chapter 7 The Contribution of Glacier Mass Balance to the TP Lake Growth in the Early 21st Century 140
7.1 Research objective 140
7.2 Data and methods 142
7.2.1 Delineating endorheic basins on the TP 142
7.2.2 Estimating lake water storage change and the uncertainty 143
7.2.3 Estimating glacier mass change and the uncertainty 146
7.2.4 Quantifying the glacier-lake mass change relationship and the uncertainty 151
7.3 The pattern of LWS changes 153
7.4 The pattern of glacier mass balance 154
7.5 Contribution of glacier mass balance to lake storage change 155
7.6 Uncertainties of glacier/lake change estimation 157
7.7 Comparison with previous estimates 159
7.8 Implications for lake and glacier change mechanisms and the relation to climate change 168
7.9 Summary 170
References 171
Chapter 8 What Drives the Rapid Water Level Recovery of the Largest Lake (Qinghai Lake) on the Tibetan Plateau over the Past Half Century? 176
8.1 Research objective 176
8.2 Description of Qinghai Lake 177
8.3 Material and methodology 178
8.3.1 LEGOS altimetry and in-situ gauged lake level datasets 178
8.3.2 Meteorological data 178
8.3.3 Reanalysis data 178
8.3.4 Glacier mass balance estimation 179
8.3.5 Lake water budget models 180
8.4 Abnormal lake water level changes of the QHL in several key years 181
8.5 Relationships between the lake level changes and hydrometeorology variables 183
8.6 Response of anomalous precipitation to the water vapor transport 184
8.7 Comparison with prior studies 188
8.8 Summary 190
References 191
Section III Impacts
Chapter 9 Ongoing Drainage Reorganization Driven by Rapid Lake Growths on the Tibetan Plateau 199
9.1 Research objective 199
9.2 Materials and methods 201
9.2.1 Study data 201
9.2.2 Lake extent mapping 201
9.2.3 Estimation of change rates of lake level and water storage 202
9.2.4 Watershed delineation on the endorheic TP 203
9.2.5 Projection of drainage reorganization occurrence and required time period 204
9.2.6 Lake-outburst flooding simulation 205
9.3 Drainage reorganizations on the endorheic TP between 2000 and 2018 206
9.4 Endorheic-exorheic transition as a chain reaction of endorheic drainage reorganization 211
9.5 Projection of future reorganization on the endorheic TP 213
9.6 Summary 216
References 217
Chapter 10 Impact of Amplified Evaporation due to Lake Expansion on the Water Budget on the Inner Tibetan Plateau 221
10.1 Research objective 221
10.2 Data and methods 222
10.2.1 Conceptual model of lake expansion-induced evaporation change 222
10.2.2 ET data and processing 222
10.2.3 Satellite data and methods of lake change mapping 226
10.2.4 Uncertainty estimation of evaporated water budgeting over newly inundated lake area 227
10.3 TP lake area changes during 2000–2015 227
10.4 Evaporation-induced water loss over expanding TP lakes 228
10.4.1 Comparison of different annual ETa data sets over ITP basins 228
10.4.2 Spatial characteristics of annual ETp data sets over ITP basins 229
10.4.3 Analyses of evaporated water loss over inundated water surface 231
10.5 The implication of evaporated water loss on the ITP 233
10.6 Uncertainty analyses on ETa and ETp estimates over ITP 234
10.6.1 Uncertainty of ETa estimation 234
10.6.2 Uncertainty of ETp estimation 235
10.7 Summary 236
References 237
Chapter 11 Wi
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