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171.
《水文科学杂志》2013,58(4):808-824
Abstract

We report results of three field campaigns conducted at 39 stations. At each station, we measured reflectance spectra in situ and collected water samples for measuring chlorophyll a (CHL) and suspended solids (SS) concentrations in the laboratory. To identify the indicative bands and develop suitable estimation models for CHL (C CHL) and SS (C SS) concentrations in Taihu Lake, a spectral-feature method and a derivative method were applied. The following conclusions were drawn: (a) the critical C CHL and C SS probably causing their spectral variation are, respectively: 0, 10, 50 and 75 μg L?1, and 0, 10, 50 and 100 mg L?1; (b) the derivative method is better than the spectral-feature method for estimating C CHL and C SS; (c) the optimal variable for CHL is a reflectance second-order derivative at 501 nm or a reflectance first-order derivative at 698 nm; the optimal variable for SS can change when its concentration is low and the range is narrow; otherwise, the optimal variable is a reflectance first-order derivative at 878 nm; and (d) the CHL and SS have an effect on one another's retrieval. The C CHL estimation accuracy would benefit from narrowing the C SS range. With C CHL increasing and its range broadening, the corresponding C SS estimation accuracy decreases gradually.  相似文献   
172.
Abstract

Abstract The geographical context and hydroclimatology of the English Lake District means that the region is an important monitor of changes to nationally significant environmental assets. Using monthly rainfall series for sites in and around the central Lake District, a continuous ~200-year precipitation index was constructed for a representative station close to Grasmere. The bridged series shows a significant decline in summer rainfall since the 1960s, offset by increases in winter and spring that are strongly linked to North Atlantic forcing. Over longer time periods, the index exhibits several notable dry (1850s, 1880s, 1890s, 1930s, 1970s) and wet (1820s, 1870s, 1920s, 1940s, 1990s) decades. These patterns are strongly reflected by reservoir inflow series and by indicators of the biological status of the region’s freshwater lakes. It is argued that long-term climate indices will become increasingly important as managers seek to evaluate recent and project environmental changes within the context of long-term natural variability.  相似文献   
173.
长江倒灌鄱阳湖原因及发生条件的量化指标   总被引:1,自引:0,他引:1       下载免费PDF全文
江湖倒灌对鄱阳湖流域水动力变化和流域水环境保护等方面有重要影响,正确认识江湖倒灌原因和倒灌发生条件对明晰江湖倒灌作用机理、研究倒灌强度和倒灌影响范围等方面具有重要意义。在剖析江湖倒灌原因的基础上,从非恒定流洪水波传播的角度出发,结合鄱阳湖为"河相"、"湖相"时江湖倒灌的特点,提出了长江作用强度指标和鄱阳湖作用强度指标,在此基础上引入江湖作用综合强度函数,依据实测资料,分析研究了江湖作用综合强度函数的关系表达式、江湖倒灌发生条件及量化指标。经验证,所提出的江水倒灌量化指标可区分江湖顶托和江湖倒灌现象,可实现对鄱阳湖为"河相"、"湖相"时的江湖倒灌预测,且提高了预测江湖倒灌起止时间、总历时和年内发生次数的准确率,成果可用于江湖关系研究和鄱阳湖流域水资源综合利用工程实践中。  相似文献   
174.
天山北坡乌鲁木齐河1号冰川与土尤克苏冰川物质平衡观察表示80年代比以前出现大的亏损。青海湖与伊赛克湖在近百年一直处于萎缩状态。从小冰期最盛时以来,乌鲁木齐河谷中冰川面积已缩去44%。上述及其他冰川与湖泊变化证据清楚地指示本世纪气候干暖化趋势增强了,并可能延续到下世纪初。但如由于CO_2及其他痕量气体增加所致的温室效应使下世纪重现全新世早、中期那样的高温,则亚洲中部有可能转为潮湿。  相似文献   
175.
青海湖沉积物中的粘土矿物   总被引:5,自引:0,他引:5       下载免费PDF全文
徐昶  林乐枝 《地质科学》1989,5(4):348-354
本文对青海湖沉积物中的粘土矿物和沉积环境进行了初步研究。沉积物的粒度成分一般以粉砂级为主,湖周沉积物较粗,湖内沉积物较细。湖中粘土矿物以伊利石-绿泥石为主,含少量蒙脱石和高岭石等。沉积物表层未见蒙脱石,粘土中Al2O3、K2O和MgO的相对百分含量的特征与海粘土的化学成分特征相似。  相似文献   
176.
The diatom biostratigraphy of the topmost sediment meter of Rotsee, Central Switzerland, is characterized by a major change fromCyclotella comensis-dominated toStephanodiscus hantzschii/S. parvus-dominated assemblages. A comparison between old phytoplankton samples, taken between 1910–1930, and subfossil diatom assemblages is used for dating the upper 35 cm of the core. There is evidence that the change in dominant diatoms occurred in 1919/20, thus before the opening of an artificial inlet in 1922, and is due to increasing eutrophication. Furthermore, the sedimentary carbonate content can be used as a good indicator for past phytoplankton productivity in Rotsee.  相似文献   
177.
Annual heat balance and equilibrium temperature of Lake Aegeri,Switzerland   总被引:1,自引:0,他引:1  
The mean heat budget of Lake Aegeri, Switzerland, is 950 MJ·m–2, comparable to that of neighbouring lakes. The annual variation in the net heat flux can be adequately described using a six-term heat balance equation based on 12 years of monthly mean meteorological and surface temperature data. Although the magnitude of the net heat flux is dominated by the radiative terms of the equation, the one-month backward shift of the net flux and total heat content extrema from the solstices and equinoxes respectively is due to the phase shift of the non-radiative with respect to the radiative terms. A linear approximation was used to express the net heat flux in terms of a heat exchange coefficient and an equilibrium temperature. The former varies from 17 to 28 W·m–2·K–1 in the course of a year; fluctuations in the latter are found to depend mainly on fluctuations in cloud cover and relative humidity, whilst the effect of fluctuations in air temperature and wind speed is slight.  相似文献   
178.
可可西里地区乌兰乌拉湖湖泊环境变迁及古人类活动遗迹   总被引:4,自引:1,他引:4  
通过对可可西里地区及在乌兰乌拉湖所发现古人类活动遗迹的综合研究,认为乌兰乌拉湖地区自晚更新世末期以来,湖泊环境发生了由湿润(3×104aB.P.以前)──温暖(2×104aB.P.前后)──干暖(1×104aB.P.以前)──冷干(1×104aB.P.以来)的变化,湖水也产生了多次进退变化,与之相适应的古人类活动也发生了迁徒变化。  相似文献   
179.
博斯腾湖流域气候及湖陆风   总被引:8,自引:0,他引:8  
王容  杜勇 《干旱区地理》1994,17(3):90-94
通过流域多个气象站的资料,分析了流域气候条件,并通过对湖区测点的气象观测资料与陆区测点- 焉耆站的同步资料对比分析,讨论了博斯腾湖区域小气候其湖陆风特征。  相似文献   
180.
应用箱状模型的理论,建立了茶卡盐湖及其外围水系的箱状模型,在测定茶卡盐湖丰水季节和枯水季节卤水的水量及流入湖区河水、泉水的流量的基础上,计算了茶卡盐湖溶洞水上渗补给湖水的平均速率,得到了满意的结果。  相似文献   
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