Relationship of underground water level and climate in Northwest China’s inland basins under the global climate change:Taking the Golmud River Catchment as an example

To identify the response of groundwater level variation to global climate change in Northwest China’s inland basins,the Golmud River Catchment was chosen as a case in this paper.Approaches of time series analysis and correlation analysis were adopted to investigate the variation of groundwater level influenced by global climate change from 1977 to 2017.Results show that the temperature in the Golmud River Catchment rose 0.57℃ every 10 years.It is highly positive correlated with global climate temperature,with a correlation coefficient,0.87.The frequency and intensity of extreme precipitation were both increased.Generally,groundwater levels increased from 1977 to 2017 in all phreatic and confined aquifers and the fluctuation became more violent.Most importantly,extreme precipitation led to the fact that groundwater level rises sharply,which induced city waterlogging.However,no direct evidence shows that normal precipitation triggered groundwater level rise,and the correlation coefficients between precipitation data from Golmud meteorological station located in the Gobi Desert and groundwater level data of five observation wells are 0.13,0.02,−0.11,0.04,and−0.03,respectively.This phenomenon could be explained as that the main recharge source of groundwater is river leakage in the alluvial-pluvial Gobi plain because of the high total head of river water and goodness hydraulic conductivity of the vadose zone.Data analysis shows that glacier melting aggravated because of local temperature increased.As a result,runoff caused groundwater levels to ascend from 1977 to 2017.Correlation coefficients of two groundwater wells observation data and runoff of Golmud River are 0.80 and 0.68.The research results will contribute to handling the negative effects of climate change on groundwater for Northwestern China.

Numerical simulation of response of groundwater flow system in inland basin to density changes

The developmental characteristics of groundwater flow system are not only controlled by formation lithology and groundwater recharge conditions,but also influenced by the physical properties of fluids.Numerical simulation is an effective way to study groundwater flow system.In this paper,the ideal model is generalized according to the fundamental characteristics of groundwater system in inland basins of Western China.The simulation method of variable density flow on the development of groundwater system in inland basins is established by using EOS9 module in TOUGHREACT numerical simulation software.In accordance with the groundwater streamline,the groundwater flow system is divided into three levels,which are regional groundwater flow system,intermediate groundwater flow system and local groundwater flow system.Based on the calculation of the renewal rate of groundwater,the analysis shows that the increase of fluid density in the central part of the basin will restrain the development of regional groundwater flow system,resulting in a decrease of the circulation rate from 32.28% to 17.62% and a certain enhancement to the local groundwater flow system,which increased from 37.29% to 51.94%.

A paleo-hydrological simulation experiment and its verification in an inland basin

Hydrological circulation,as the most basic material cycle and active natural phenomenon on earth,exerts a significant in fluence on climate change.The mid-Holocene is an important period to better understand modern environmental change;however,little research has focused on its quantitative simulation of paleo-hydrological process.In this research,we first collected chronological evidence and sediment records from six Holocene sedimentary sections in the Shiyang River Ba sin to reconstruct the mid-Holocene environment and terminal paleo-lake area.Secondly,we comprehensively analyzed modern pollen combinations and their propagation characteristics in surface soil,air,river and lacustrine sediments in the Shiyang River Basin,and combined the pollen records,as well as quantitatively reconstructed the millennial-scale vegeta tion zones.Finally,based on the land-cover adjustment results during the mid-Holocene,we successfully used the Soil and Water Assessment Tool(SWAT)model,a modern distributed hydrological watershed model,to simulate mid-Holocene runoff in the basin.Results show that the reconstructed climate in the basin was warmer and moister than that in recent times.Vegetation types in the mid-Holocene mainly consisted of sub-alpine shrub distributed between 2,550 m and 2,750 m,forest at an elevation of 2,550 2,750 m,steppe at an elevation of 1,550 2,150 m and desert steppe below 1,550 m.The up stream,midstream,downstream and average annual runoff of the mid-Holocene in the basin were 16.76×10^8 m^3,22.86×10^8 m^3,9.00×10^8 m^3 and 16.20×10^8 m^3 respectively,compared to 15.61×10^8 m^3 of modern annual runoff.Also,the area of terminal paleo-lake in the mid-Holocene was 628 km^2.Thus,this study provides a new quantitative method for paleo-hy drological simulation.

Mutual optimization of water utilization structure and industrial structure in arid inland river basins of Northwest China

Water is a key restricting factor of the economic development and eco-environmental protection in arid inland river basins of Northwest China. Although water supplies are short, the water utilization structure and the corresponding industrial structure are unbalanced. We constructed a System Dynamic Model for mutual optimization based on the mechanism of their interaction. This model is applied to the Heihe River Basin where the share of limited water resources among ecosystem, production and human living is optimized. Results show that, by mutual optimization, the water utilization structure and the industrial structures fit in with each other. And the relationships between the upper, middle and lower reaches of the Heihe River Basin can be harmonized. Mutual benefits of ecology, society and economy can be reached, and a sustainable ecology-production-living system can be obtained. This study gives a new insight and method for the sustainable utilization of water resources in arid inland river basins.

Simulation of hydrological processes of mountainous watersheds in inland river basins: taking the Heihe Mainstream River as an example

The hydrological processes of mountainous watersheds in inland river basins are complicated.It is absolutely significant to quantify mountainous runoff for social,economic and ecological purposes.This paper takes the mountainous watershed of the Heihe Mainstream River as a study area to simulate the hydrological processes of mountainous watersheds in inland river basins by using the soil and water assessment tool(SWAT)model.SWAT simulation results show that both the Nash–Sutcliffe efficiency and the determination coefficient values of the calibration period(January 1995 to December 2002)and validation period(January 2002 to December 2009)are higher than 0.90,and the percent bias is controlled within±5%,indicating that the simulation results are satisfactory.According to the SWAT performance,we discussed the yearly and monthly variation trends of the mountainous runoff and the runoff components.The results show that from 1996 to 2009,an indistinctive rising trend was observed for the yearly mountainous runoff,which is mainly recharged by lateral flow,and followed by shallow groundwater runoff and surface runoff.The monthly variation demonstrates that the mountainous runoff decreases slightly from May to July,contrary to other months.The mountainous runoff is mainly recharged by shallow groundwater runoff in January,February,and from October to December,by surface runoff in March and April,and by lateral flow from May to September.

SUSTAINABLE EXPLOITATION AND UTILIZATION OF WATER RESOURCES IN THE INLAND RIVERBASIN OF ARID NORTHWEST CHINA

Calculated in terms of surface runoff plus irrepeated groundwater, there is about 8. 67 ×1010m3 of total available water resources in the inland river basins of arid Northwest China. Water resources is the decisive factor for survival of oases and human being. But there have arisen several aspects of Serious eco-environment problems resulted from irrational exploitation and utilization. From now on, the development and utilization of water not only requires to promote regional economy, but also needs to protect and improve the environment based on their potential. Sustainable utilization needs to broaden new sources and saving water at first. Then three measures are recommended.

Study of temperature and precipitation change in upstream mountain area of the Hexi inland river basin since 1960s

All rivers in the Hexi inland region of Gansu Province, China, originate from the northern slope of the Qilian Mountains. They are located in the southern portion of the region and respectively belong to the three large river systems from east to west, the Shiyang, Heihe and Shule river basins. These rivers are supplied by precipitation, snowmelt and ice-melt runoff from the Qilian Mountain area. Therefore, changes of precipitation and temperature in the upstream watersheds of these rivers have an important effect on changes of mountainous runoff and reasonable utilization of water resources in this region. For this reason, the Qilian Mountain area, upstream watersheds and runoff forming areas of these rivers are chosen as the study area. The change characteristics and variation trend of temperature and precipitation in this area under the backdrop of global warming axe analyzed based on observa- tional data of relational weather and hydrologic stations in the area. Results show that temperatures in the upriver mountain areas of these three large river basins have been increasing, although the increasing degree is differentially affected by global warming. The rising extent of annual and seasonal temperatures in the upstream mountain area of the Shule river basin located in the west- em Qilian Mountains, were all largest over the past 50 years. Precipitation in the upstream mountain areas of Hexi region＇ three river basins located respectively in the western, middle and eastern Qilian Mountains have been presenting an increasing trend to varying degrees as a whole for more than 50 years. This means that climate in the upstream mountain areas of Hexi region＇ three river basins are becoming increasingly warmer and moister over the past 50 years, which will be very good for the ecological en- vironment and agricultural production in the region.

Hydrological and water cycle processes of inland river basins in the arid region of Northwest China

The increasing shortage in water resources is a key factor affecting sustainable socio-economic development in the arid region of Northwest China(ARNC). Water shortages also affect the stability of the region's oasis ecosystem. This paper summarizes the hydrological processes and water cycle of inland river basins in the ARNC, focusing on the following aspects: the spatial-temporal features of water resources(including air water vapor resources, runoff, and glacial meltwater) and their driving forces; the characteristics of streamflow composition in the inland river basins; the characteristics and main controlling factors of baseflow in the inland rivers; and anticipated future changes in hydrological processes and water resources. The results indicate that:(1) although the runoff in most inland rivers in the ARNC showed a significant increasing trend, both the glaciated area and glacial ice reserves have been reduced in the mountains;(2) snow melt and glacier melt are extremely important hydrological processes in the ARNC, especially in the Kunlun and Tianshan mountains;(3) baseflow in the inland rivers of the ARNC is the result of climate change and human activities, with the main driving factors being the reduction in forest area and the over-exploitation and utilization of groundwater in the river basins; and(4) the contradictions among water resources, ecology and economy will further increase in the future. The findings of this study might also help strengthen the ecological, economic and social sustainable development in the study region.

A distributed runoff model for inland mountainous river basin of Northwest China

In order to predict the futuristic runoff under global warming, and to approach to the effects of vegetation on the ecological environment of the inland river mountainous watershed of Northwest China, the authors use the routine hydrometric data to create a distributed monthly model with some conceptual parameters, coupled with GIS and RS tools and data. The model takes sub-basin as the minimal confluent unit, divides the main soils of the basin into 3 layers, and identifies the vegetation types as forest and pasture. The data used in the model are precipitation, air temperature, runoff, soil weight water content, soil depth, soil bulk density, soil porosity, land cover, etc. The model holds that if the water amount is greater than the water content capacity, there will be surface runoff. The actual evaporation is proportional to the product of the potential evaporation and soil volume water content. The studied basin is Heihe mainstream mountainous basin, with a drainage area of 10,009 km 2 . The data used in this simulation are from Jan. 1980 to Dec. 1995, and the first 10 years' data are used to simulate, while the last 5 years' data are used to calibrate. For the simulation process, the Nash-Sutcliffe Equation, Balance Error and Explained Variance is 0.8681, 5.4008 and 0.8718 respectively, while for the calibration process, 0.8799, -0.5974 and 0.8800 respectively. The model results show that the futuristic runoff of Heihe river basin will increase a little. The snowmelt, glacier meltwater and the evaportranspiration will increase. The air temperature increment will make the permanent snow and glacier area diminish, and the snowline will rise. The vegetation, especially the forest in Heihe mountainous watershed, could lead to the evapotranspiration decrease of the watershed, adjust the runoff process, and increase the soil water content.

The Process of Cultivated Land and Water Resource Distribution Changing in Recent Decades in Upstream and Downstream in Shiyang Inland River Basin in Arid Area of Northwest China

Last century 50 - 70 years, the dam construction of Shiyang Inland River Basin (SIRB) profound impact on the distribution of water resources and arable land in the basin. Through data collection, field surveys and remote sensing image interpretation, we analysis the use of land and water resources change process in the middle and lower reaches of SIRB in recent decades. The results show: (1) The cultivated area of SIRB has been an upward trend in recent decades, The whole basin cultivated area has increased total 229,000 hm2 from 1973 to 2010 and mainly in the middle and lower reaches. Midstream increased by 149,700 hm2 accounting for 65.36 percent of total, downstream increased by 70,000 hm2 accounting for 30.70 percent of total. (2) The amount of surface water resources of downstream reduce significantly gradually since dam construction, and the water table sharp decline. While the volume of surface water resources come downstream from the 1950s accounted for 30 to 40 percent of the total gradually reduced to less than 10% in 2012;(3) since the arable land area of middle and lower reaches of SIRB basin substantial increase, so the surface water resource does not meet irrigation needs. Agricultural irrigation relies heavily on exploitation of groundwater to supplement, resulting in Regional Groundwater Depth dropped rapidly, and forming several huge funnel groundwater settlements. 20 years from 1981 to 2001 the groundwater level of midstream dropped from around 5m to around 10m in Wuwei, and in Minqin dam-region of downstream along faster rate of decline in 20 years fell from 8.52 m to 22.68 m. Dam construction project has changed the pattern of the basin water cycle, the middle reaches closure a large number of surface water resources led to downstream sharp decline. Downstream continued exploitation of groundwater formed a few huge funnel groundwater settlements, it caused serious ecological problems. The basin should adjust the industrial structure and develop water saving irrigation, promote a virtuous cycle of water resources, to achieve sustainable development, seek a sustainable development ways conversion natural oasis to artificial oasis efficiency in arid zone.

基于生态水文最优性理论的河西内陆河流域植被覆盖模拟

在生态恢复过程中,生态系统中植被所处状态对于生态平衡是否可持续至关重要,本研究以河西内陆河流域2000-2020年生长季气象和植被数据为基础,应用Eagleson生态水文最优性理论,模拟流域内生态水文平衡状态下的最优植被覆盖度Meq,植被覆盖度恢复阈值与当前现状植被覆盖度的差值即为植被恢复潜力。结果表明:1)模拟的多年平均最优植被覆盖度Meq与多年生长季平均实际植被覆盖度M的变化一致,但过渡更加平稳,呈现从东南向西北递减的趋势,流域内多年生长季平均实际植被覆盖度为0.163,模拟的多年平均最优植被覆盖度为0.166。2)流域内平均恢复潜力为0.003,植被覆盖度仍具有恢复潜力的面积占比为62.76%,分布在流域北部地区,3个流域内平均植被恢复潜力为石羊河流域>黑河流域>疏勒河流域。3)河西内陆河流域植被恢复潜力与区域干旱指数密切相关。森林的平均植被恢复潜力随着干旱等级增加呈减小的变化特征;而灌木植被覆盖度超过恢复潜力的程度随干旱指数增加呈先加剧后减轻的变化特征。

内蒙古草原内陆河流域水文循环要素时空演变及驱动因素

[目的]开展内蒙古草原内陆河流域水文循环要素对植被动态和气候变化的响应研究,对于内蒙古草原内陆河流域的生态保护及区域水资源开发利用具有重要的理论意义。[方法]以内蒙古草原内陆河流域为研究区,基于多源遥感、气候气象、水文等数据,采用趋势检验、显著性检验和相关性分析等方法,对流域水文循环要素的时空演变及驱动因素进行相关分析。[结果](1)流域蒸散发呈显著上升趋势(0.994 mm/a),降水量呈显著下降趋势(2.69 mm/a),土壤水分呈增加趋势,其中子流域锡林河径流呈下降趋势,巴拉格尔河径流呈上升趋势;(2)生长季植被总体呈增加趋势,植被归一化指数(NDVI)、总初级生产力(GPP)和叶面积指数(LAI)整体呈东高西低的阶梯状空间分布格局,气温整体呈现上升趋势;(3)植被变化与蒸散发(ET)、土壤水分(SSM)呈正相关,气温和蒸散发整体上呈现显著正相关(R=0.699,p=0.01),空间相关性由西向东递增;气温和径流呈负相关,和土壤水分在流域东、西部呈显著负相关性。[结论]流域水文循环变量(降水、蒸散发、土壤水分、径流量)随着植被增加而增加;降水、土壤水分和径流量随气温上升而减少,蒸散发随气温上升而增加。

甘肃省河西内陆河实测出山径流量变化及其影响因素分析

甘肃省河西内陆河流域水资源极其短缺,流域内中西部和东部水系出山径流变化存在一定差异,研究出山径流量的变化情况及不同因素的贡献率,对保障区域水资源可持续开发利用具有重要意义。基于1956-2021年出山径流及主要产流区降水、气温资料,采用多种趋势和突变检验法、累积量斜率变化率法,结合径流补给特征,解析三大水系出山径流变化及其对降水、气温变化的响应情况,结果表明:(1)石羊河水系多年平均出山径流量13.60亿m^(3),历年呈不显著减少趋势,降水呈不显著增加趋势,气温显著升高使蒸发量增加,致使径流呈减少趋势;(2)黑河水系多年平均出山径流量由突变点2006年前的30.62亿m^(3)增加为突变点后的35.60亿m^(3),降水对径流变化的贡献率为16.7%,气温显著升高,对径流变化的影响增强;(3)疏勒河水系多年平均出山径流量由突变点1998年前的14.22亿m^(3)增加为突变点后的17.93亿m^(3),降水和气温对径流变化的影响相当,贡献率分别为30.4%、30.2%。河西内陆河三大水系径流补给特征、气候条件存在一定差异,致使径流对不同驱动因素的响应情况也不一致。

河西内陆河流域生态屏障建设综合评价与提升策略研究

生态屏障建设是推进人与自然和谐共生的中国式现代化的重要手段,内陆河流域生态屏障建设评价对于总结生态屏障建设成效与问题及落实中国式现代化建设战略任务具有重要意义。基于社会—生态耦合视角,在构建生态屏障建设评价指标体系基础上,运用综合指数法,对2015—2020年河西内陆河流域生态屏障建设状况进行了动态综合评价,并据此提出提升策略。结果表明:(1)河西内陆河流域生态屏障建设综合指数呈小幅上升态势,生态屏障建设处于发展提升阶段,流域生态安全多处于一般和较差状态;(2)流域生态屏障建设成效空间上整体呈现出自西往东逐渐下降的趋势,其中张掖市生态屏障建设成效明显,生态屏障建设综合指数稳步提升。基于上述研究,建议从社会—生态系统整体性出发,将生态屏障建设融入流域建设全过程,在生态产业、生态文化和生态社会等方面进行整体谋划和系统安排,统筹推进流域生态屏障建设转型提升。

内蒙古内陆河流域地下水资源评价及相关地质环境问题分析

【研究目的】为提升对内蒙古内陆河流域水文地质和地下水资源的认知程度,提高地下水资源利用效率,减少地质环境问题。【研究方法】本文以内蒙古内陆河流域为主要工作区,查明了该流域的补径排特征及水文地质条件,收集并整理了该流域近20年来的气象及地下水开发利用等相关资料,更新了地下水资源评价相关水文地质参数,对该流域地下水资源补排项进行汇总分析,对流域内山丘区和平原区分别采用排泄量法和补给量法进行地下水资源评价。同时全面论述了该流域地下水动态变化特征,并探讨了与地下水相关的湖泊萎缩、土地荒漠化等生态地质环境问题。【研究结果】计算得出内陆河流域地下水资源总量为37.94亿m^(3),年际上坝上地区浅层地下水位大致经历了先升高后降低的总趋势,地下水位年内总体呈现周期性波动的趋势,受地下水位影响流域内湖泊萎缩严重,沙质荒漠化面积减小,而盐碱质荒漠化逐渐加剧。【结论】该研究为该区水资源的可持续开发利用与生态环境保护提供了基础资料和科学依据。

高寒内陆河流域水文水环境地表蒸散发量时空变异规律研究——以巴音河流域为例

蒸散发是连接土壤-植被-大气间水热交换的最重要环节,是水循环模拟、地表过程模拟的关键参数.本研究基于巴音河流域气象、下垫面数据建立SWAT(Soil and Water Assessment Tools)模型,利用流域径流观测数据对其进行校准后提取各子流域蒸散发量,用以验证同时空尺度GLEAM(the Global Land Evaporation Amsterdam Model)v3数据集的精度.最终在保证GLEAM v3数据集适用性的前提下探讨了巴音河流域地表蒸散发量、土壤蒸发量和植物散发量的时空变异规律.结果表明:(1)GLEAM在巴音河流域的适用性良好,月尺度上其模拟的地表蒸散发量与SWAT模型模拟的相应子流域蒸散发量的R^(2)>0.87,NSE>0.81,|PBIAS|<2;(2)在空间上,巴音河流域多年平均地表蒸散发量(140~269mm)、土壤蒸发量(98~135mm)及植物散发量(22~129mm)均表现出由东北部高海拔山区到西南部山前平原逐渐递减的分布特征;(3)地表蒸散发量、土壤蒸发量和植物散发量在季节上的空间分布特征除冬季外亦基本呈现由东北部高海拔山区到西南部山前平原逐渐递减的分布特征;(4)地表蒸散发量、土壤蒸发量及植物散发量的逐年变化趋势与流域降水量的变化趋势相同,三者的多年月平均值和多年日平均值呈现出明显的季节特征,峰值出现在7月,最低值出现在12月,各个时间尺度上土壤蒸发量均大于植物散发量.

Impacts of land use changes on groundwater resources in the Heihe River Basin

Land use and land cover changes have a great impact on the regional hydrological process. Based on three periods of remote sensing data from the 1960s and the long-term observed data of groundwater from the 1980s, the impacts of land use changes on the groundwater system in the middle reach of Heihe River Basin in recent three decades are analyzed by the perspective of groundwater recharge and discharge system. The results indicate that with the different intensities of land use changes, the impacts on the groundwater recharge were 2.602 × 10^8 m^3/a in the former 15 years （1969-1985） and 0.218 × 10^8 m^3/a in the latter 15 years （1986-2000）, and the impacts on the groundwater discharge were 2.035 × 10^8 m^3/a and 4.91 × 10^8 m^3/a respectively. When the groundwater exploitation was in a reasonable range less than 3.0 × 10^8 m^3/a, the land use changes could control the changes of regional groundwater resources. Influenced by the land use changes and the large-scale exploitation in the recent decade, the groundwater resources present apparently regional differences in Zhangye region. Realizing the impact of land use changes on groundwater system and the characteristics of spatial-temporal variations of regional groundwater resources would be very important for reasonably utilizing and managing water and soil resources.

Response of Glacier and Lake Covariations to Climate Change in Mapam Yumco Basin on Tibetan Plateau during 1974-2003

The study of spatial and temporal covariances of glaciers and lakes would help us to understand the impact of climate change within a basin in Tibet. This study focuses on glacier and lake variations in the Mapam Yumco （玛旁雍错） basin （covering 7 786.44 km^2） by integrating series of spatial data from topographic maps and digital satellite images at four different times： 1974, 1990, 1999, and 2003. The results indicate that： （1） decreased lakes, retreated glaciers, enlarged lakes and advanced glaciers co-exist in the basin during the last 30 years; （2） glacier recession was accelerated in recent years due to the warmer climate; （3） lake areas in the basin are both reduced and enlarged by an accelerated speed with more water supplies from speeding melt glaciers or frozen ground in the last three decades.

WRF-Hydro模型参数在河西内陆河流域的敏感性分析

为研究WRF-Hydro模型参数在河西内陆河流域的敏感性,以西营河流域九条岭水文站以上区域为研究区,在离线模式下利用2015—2018年的全球预报系统(GFS)数据驱动WRF-Hydro模型。基于LH-OAT方法对WRF-Hydro模型的6个主要参数对不同评价指标和空间分辨率的汇流演算网格的敏感性进行了分析,定量计算了各参数的敏感性指标,划分了敏感度等级,并结合典型洪水分析了各参数对洪水过程线的具体影响。结果表明:河道曼宁糙率乘子(MANNFAC)为极敏感参数,入渗系数(REFKDT)、土壤饱和导水率(REFDK)、深层导水系数(slope)为敏感参数,地表糙率乘子(OVROUGHRTFAC)为一般敏感参数,地表持水深度乘子(RETDEPRTFAC)为不敏感参数;各参数的敏感性并不是一成不变的,参数敏感度会受到评价指标的影响,有一定程度的变化;随着汇流演算网格空间分辨率的变化,各参数全局敏感度也会有小幅变化,但参数的全局敏感度等级不发生改变;MANNFAC对峰现时间的调节效果最好,REFKDT和REFDK对洪量和洪峰流量的调节效果显著,slope可以很好地调节洪水过程线的形状。

Sentinel-2和ICESat-2密集时序数据反演浅平型内陆湖泊水量变化

干旱区内陆尾闾湖泊由于湖盆地形浅平、岸线复杂等特点,采用传统的水位-面积关系法难以反演高精度的水量变化信息。本文提出了一种基于密集时序ICESat-2和Sentinel-2数据反演浅平型内陆湖泊湖盆地形和重建水量时序的方法。本文方法利用浅平型湖泊季节性变化显著的特性,筛选和计算不同时期湖盆内非水面区域的所有ICESat-2激光光子点的高程信息,并根据水面等高的特性内插得到Sentinel-2不同时相水面线的高程信息,在此基础上通过这些加密的高程点构建高精度湖盆地形信息,并结合水面时序重建湖泊的水量变化。以新疆塔里木河尾闾台特玛湖为试验区,基于132期Sentinel-2卫星影像和28个时相的ICESat-2激光脉冲数据,重建了2016—2022年的湖泊水量时序。结果表明,本文方法获取的湖盆地形高程中误差为0.103 m,可为无资料浅平型湖泊水量信息的时序重建提供一种思路。