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1.
This study explores the microphysical responses to a cloud seeding operation in the Sanjiangyuan region, China. The cloud seeding was performed using a zigzag flight pattern, while the detection phase was accomplished using a back-and-forth flight pattern through the top of a stratocumulus layer. Global Position System（GPS） and Particle Measuring System（PMS） data obtained during the operation are used to determine the efective cloud area before and after the operation, diferentiate the phase states of cloud particles, and analyze changes in the concentrations of liquid cloud particles and ice crystals, the evolution of the cloud particle spectrum, and the content of supercooled water. The median diameter of liquid cloud particles in the area of the cloud-seeding operation was 3.5–18.5 μm, most cloud particles observed in the 21.5–45.5-μm size regime were ice crystals, while all particles of size 50 μm and above were in the ice phase. Changes in the concentration and typical diameter of cloud particles within 36 km downwind of the cloudseeding operation did not exceed natural fluctuations in the cloud area before the operation; however, the concentration of liquid cloud particles decreased substantially in areas with high concentrations of supercooled water（concentrations of supercooled water exceeding 0.01 g m 3）. The concentration of ice crystals within the measuring range of the Forward Scattering Spectrometer Probe（FSSP） increased substantially, the water content of ice-phase particles increased, and the average supercooled water content in the cloud decreased from（68.3± 23.1）% before the operation to（34.2± 12.4）%. The efects of cloud seeding were more pronounced in parts of the cloud where the content of supercooled water was higher. Little to no efects were observed in parts of the cloud with low concentrations of supercooled water. 相似文献
2.
三江源地区秋季典型多层层状云系的飞机观测分析 总被引：4，自引：0，他引：4
利用三江源地区一次机载粒子测量系统PMS(Particle Measuring Systems)的分层垂直探测资料,系统研究了该地区秋季典型多层层状云系的微物理特性,结果表明:(1)云系由4层云层组成,Cs(卷层云)和上层As(高层云)为冰云,下层As和Sc(层积云)为过冷混合态云。下层As的云粒子浓度和过冷水含量最大,Sc的云粒子尺寸及谱宽最大,且具有较明显的地区特性;(2)Sc(下层As及对流泡)中中值直径在3.5～18.5 μm(3.5～ 21.5 μm)之间的云粒子为液相,中值直径大于21.5 μm(24.5 μm)的云粒子为冰相;(3)混合态云中高过冷水区与低过冷水区云的粒子谱分布差异明显,Sc高过冷水区有较明显的淞附增长现象;(4)Sc、下层As云底、对流泡顶高过冷水区的云滴有效半径依次增加。Sc高过冷水区的过冷水含量比率均值及标准差为69.9±19.4%,且与过冷水含量存在一定的关联性;下层As云底高过冷水区的过冷水含量比率无明显变化,其均值及标准差为89.2±8.1%;(5)混合态云各高度层FSSP(前向散射粒子谱探头)平均粒子谱均为单峰型伽玛分布,混合态云和冰云各高度层2DC(二维灰度云粒子探头)平均粒子谱基本上都为负指数型分布。 相似文献
3.
三江源生态保护和建设一期工程生态成效评估 总被引：11，自引：2，他引：9
邵全琴 樊江文 刘纪远 黄麟 曹巍 徐新良 葛劲松 吴丹 李志强 巩国丽 聂学敏 贺添 王立亚 邴龙飞 李其江 陈卓奇 张更权 张良侠 杨永顺 杨帆 周万福 刘璐璐 祁永刚 赵国松 李愈哲 《地理学报》2016,71(1):3-34
基于生态系统结构--服务动态过程趋势分析,针对生态保护与建设工程预期目标,构建了由生态系统结构,质量,服务及其变化因素构成的生态成效评估指标体系,研究发展野外观测,遥感监测和生态过程定量模拟一体化的监测评估技术体系,评估了三江源生态保护和建设一期工程的生态成效.结果表明:工程实施8年以来,三江源区宏观生态状况趋好但尚未达到1970s比较好的生态状况,草地持续退化趋势得到初步遏制但难以达到预期"草地植被盖度提高平均20%~40%"的目标,水体与湿地生态系统整体有所恢复,生态系统水源涵养和流域水供给能力提高,区域水源涵养量达到了增加13.20亿m3目标;重点工程区内生态恢复程度好于非工程区,除了气候影响以外,工程的实施对促进植被恢复具有明显而积极的作用;然而,草地退化局面没有获得根本性扭转,工程实施尚未遏制土壤水蚀增加趋势,一期工程局部性和初步性特点突显出三江源区生态保护任务的长期性和艰巨性. 相似文献
4.
“三江源”夏季降水异常与大气环流异常的关系 总被引：1，自引：0，他引：1
利用三江源地区14个站1961-2005年逐月降水资料,对全区近45年夏季降水异常的时空特征及与大气环流异常的关系进行了分析.结果表明,近45年来,三江源地区的夏季降水量具有良好的空间一致性,总体呈微弱的减少趋势,减少幅度为9mm/45a;三江源地区经历了5个干、湿交替的阶段,存在较明显的准2年、准4～6年的振荡周期,自1980年代中期后12～14年左右的周期信号较强;1968、1979及1986年是3个明显的气候突变点,小波分析结果与降水序列大-小-大-小-大的变化趋势及突变检验存在良好的对应关系.环流分析表明,三江源地区夏季旱、涝年份的大气环流配置形势在高度距平场、风场和温度场均呈反向变化,可作为强信号,对三江源夏季降水的异常预测起指示作用. 相似文献
5.
Willingness to Pay (WTP), Willingness to Work (WTW) and Willingness to Accept Compensation (WTA) are the three quantitative criteria for assessing local ecological asset values for the social aspects of ecosystem services and residents’ willingness to contribute to and receive compensation for tourism ecology. The objectives of this study are to estimate the residents’ willingness to pay, work and accept compensation for conservation at Sanjiangyuan National Park, and to analyze the relationship between residents’ attitude towards tourism ecology and the ecological assets of the National Park based on a standard questionnaire survey. The dichotomous choice Contingent Valuation Method (CVM) was employed to determine the willingness. The survey conducted in 2018 collected WTP, WTW, WTA, socio-demFographical information, social trust and resident perceptions toward tourism impacts and relevant management strategies from 244 residents in two counties. Based on generalized linear modeling, income and education level are important for residents’ WTP and WTA, but other social characteristics, such as gender and age, do not have significant effects. The social trust is found to be a significant factor on residents’ willingness, despite the limitation on education level. Also, government funding is associated with residents’ inclination to WTP, WTW and WTA, but the support levels differ among the two counties due to geographical and social heterogeneities. The estimated WTP, WTW and WTA for the Sanjiangyuan National Park in 2018 were 1.2448×10 7 yuan, 1.247×10 6 hours and 2.3232×10 7 yuan yr -1 based on the survey and published demographics. This study, for the first time, estimates the WTP, WTW and WTA for the Sanjiangyuan National Park and informs ecological conservation managers and policy makers. Ultimately, to maintain the long-term benefits arising from sustainable development, compensation should be specifically tailored and site-dependent, and development measures based on local resources should be adopted by governments to actively support eco-tourism activities. 相似文献
6.
基于Google Earth Engine平台的三江源地区生态环境质量动态监测与分析 总被引：2，自引：0，他引：2
三江源是中国陆地生态系统最脆弱和敏感的区域之一,一旦遭到破坏则不可逆转。受三江源地区多云等不利气象条件的影响,很难获取大范围尺度上季相一致的、无云的Landsat遥感影像。本文利用Google Earth Engine平台,对1990-2015年的相同季节的3766景Landsat影像进行像元级融合并重构最小云量影像集,借助GEE的并行云端计算,快速得到了能够反映生态环境质量的遥感生态指数（RSEI）,对三江源地区的生态环境质量进行了评价与监测。三江源时空变化与差异分析表明：1990-2000年生态环境质量呈快速下降状态,RSEI平均值从0.588下降到了0.505,生态环境质量变化以轻度恶化为主;2000-2015年生态环境质量下降速度变缓,并于2015年呈现变好态势,生态环境质量变化以不变为主,且轻度恶化面积大幅减少;该地区的生态环境状况呈现出空间分异,自西向东,生态状况变差。基于GEE平台在三江源地区的实验结果表明,GEE可以作为大区域范围的生态环境质量评价与监测的计算平台。 相似文献
7.
近30年来青海省三江源区草地的土壤侵蚀时空分析 总被引：5，自引：0，他引：5
分析了青海省三江源区草地生态系统土壤侵蚀的空间差异,以及草地退化与土壤侵蚀的关系,并对该区近30年来土壤侵蚀的动念变化进行描述.结果表明,该区域微度以上土壤侵蚀面积占源区总面积的46.47%,而草地生态系统发生微度以上土壤侵蚀的面积比例达56.04%.源区土壤侵蚀类型是以冻融侵蚀伴随着水力侵蚀或风力侵蚀的复合侵蚀为主,... 相似文献
8.
2005-2009年三江源自然保护区生态保护和建设工程生态成效综合评估 总被引：6，自引：1，他引：5
本文评价了三江源自然保护区生态系统宏观结构及涵养水源、保持水土、保护生物多样等主要生态服务功能,分析了自然保护区生态保护与建设工程的生态成效及其原因。结果显示,工程实施后,各自然保护区的土地覆被转类指数明显增加,生态系统宏观状况好转;保护区内草地生产力皆呈增加趋势,水域面积增加,食物供给能力提高,栖息地生境好转。森林类保护区的森林面积减少趋势得到遏制;湿地类保护区的湿地面积多呈增加趋势;草地类保护区的草地减少趋势缓解,荒漠化明显遏制,草地植被覆盖度有所增加;冰川类保护区多条冰川出现明显退缩导致冰川融水增多,有利于雪线以下草地净初级生产力的增加。 相似文献
9.
三江源地区草地生态系统服务价值评估 总被引：5，自引：0，他引：5
三江源地区的草地生态系统对于维持区域生态平衡和保障社会经济可持续发展具有重要意义。本文基于千年生态系统评估(Millennium Ecosystem Assessment, MA)的生态系统服务分类体系, 采用多种方法对三江源草地生态系统的9 项服务价值逐项进行了评估, 得出2000 年三江源草地生态系统服务价值为562.60 亿元, 其中价值最高的两种服务类型依次为气候调节和食物生产, 分别达259.09 亿元和111.68 亿元, 贡献率分别为46.05%、19.85%。按照草地类型划分, 高寒草甸和高寒草原服务价值分别为490.95 亿元、64.68 亿元, 占总服务价值的87.42%和11.52%。虽然沼泽单位面积服务价值最高, 为4230.77 元/hm2, 但在草地生态系统面积中所占比例较低, 总价值相对很低。本文关于三江源草地生态系统的评估结果可以为制定区域生态保护和生态补偿政策提供科学支撑。 相似文献
10.
Simulation of Effects of Grassland Degradation on Regional Climate over Sanjiangyuan Region in Qinghai-Tibet Plateau 总被引：1，自引：0，他引：1 
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下载免费PDF全文 Regional climate model （RegCM3） was applied to explore the possible effects of land use changes （e.g., grassland degradation in this study） on local and regional climate over the Sanjiangyuan region in the Qinghai-Tibet Plateau. Two multiyear （1991-1999） numerical simulation experiments were conducted： one was a control experiment with current land use and the other was a desertification experiment with potential grassland degradation. Preliminary analysis indicated that RegCM3 is appropriate for simulating land- climate interactions, as the patterns of the simulated surface air temperature, the summer precipitation, and the geopotential height fields are consistent with the observed values. The desertification over the Sanjiangyuan region will cause different climate effects in different regions depending on the surrounding environment and climate characteristics. The area with obvious change in surface air temperature inducing by grassland degradation over the Sanjiangyuan region is located in the Qinghai-Tibet Plateau. A winter surface air temperature drop and the other seasons＇ surface air temperature increase will be observed over the Qinghai-Tibet Plateau based on two numerical simulation experiments. Surface air temperature changes in spring are the largest （0.46℃）, and in winter are the smallest （smaller than 0.03℃）, indicating an increasing mean annual surface air temperature over the Qinghai-Tibet Plateau. Surface air temperature changes will be smaller and more complex over the surrounding region, with minor winter changes for the regions just outside the plateau and notable summer changes over the north of the Yangtze River. The reinforced summer heat source in the plateau will lead to an intensification of heat low, causing the West Pacific subtropical high to retreat eastward. This will be followed by a decrease of precipitation in summer. The plateau＇s climate tends to become warm and dry due to the grassland degradation over the Sanjiangyuan region. 相似文献