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1966—2015年天山南北坡空气湿度差异及其影响因素 被引量:12
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作者 陈迪桃 黄法融 +1 位作者 李倩 李兰海 《气候变化研究进展》 CSCD 北大核心 2018年第6期562-572,共11页
利用天山地区近50年(1966—2015年)逐日气象资料,采用Mann-Kendall趋势检验法研究了天山南北坡相对湿度(RH)的时空变化特征,分析了天山南北坡RH对平均气温、降水量、平均风速、参考蒸散量、日照时数的敏感性,并探讨了引起RH变化的主导... 利用天山地区近50年(1966—2015年)逐日气象资料,采用Mann-Kendall趋势检验法研究了天山南北坡相对湿度(RH)的时空变化特征,分析了天山南北坡RH对平均气温、降水量、平均风速、参考蒸散量、日照时数的敏感性,并探讨了引起RH变化的主导因素。结果表明:(1)整个天山地区RH变化有略微上升的趋势但不显著,北坡RH总体呈下降趋势,南坡RH总体呈上升趋势。(2) RH空间分布呈自北向南递减趋势,南北坡全年及春季以下降趋势为主,而夏、秋、冬三季均以上升趋势为主,且南坡变化趋势的显著性高于北坡。(3) RH对风速、气温、日照时数及参考蒸散量均为负敏感,对降水量为正敏感。北坡RH对各气象因子的敏感程度依次为日照时数>参考蒸散量>风速>气温>降水量,南坡敏感程度依次为日照时数>风速>参考蒸散量>气温>降水量。空间分布上,仅降水量敏感系数高值区位于北坡伊犁河谷,其余要素敏感系数高值区均位于南坡。(4)参考蒸散量是影响天山地区RH变化的主导因子,整个天山地区参考蒸散发贡献率较高,日照时数贡献率高值区集中于北坡伊犁河谷,风速、降水量、气温贡献率高值区均集中于南坡克孜勒苏地区。 展开更多
关键词 天山南北坡 相对湿度(RH) 差异 Mann-Kendall趋势检验法 敏感性分析
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Avalanche activity and characteristics of its triggering factors in the western Tianshan Mountains,China 被引量:11
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作者 HAO Jian-sheng huang fa-rong +2 位作者 LIU Yang Amobichukwu Chukwudi AMANAMBU LI Lan-hai 《Journal of Mountain Science》 SCIE CSCD 2018年第7期1397-1411,共15页
Snow avalanche is a serious threat to the safety of roads in alpine mountains. In the western Tianshan Mountains, large scale avalanches occur every year and affect road safety. There is an urgent need to identify the... Snow avalanche is a serious threat to the safety of roads in alpine mountains. In the western Tianshan Mountains, large scale avalanches occur every year and affect road safety. There is an urgent need to identify the characteristics of triggering factors for avalanche activity in this region to improve road safety and the management of natural hazards. Based on the observation of avalanche activity along the national road G218 in the western Tianshan Mountains, avalanche event data in combination with meteorological, snowpack and earthquake data were collected and analyzed. The snow climate of the mountain range was examined using a recently developed snow climate classification scheme, and triggering conditions of snow avalanche in different snow climate regions were compared. The results show that snowfall is the most common triggering factor for a natural avalanche and there is high probability of avalanche release with snowfall exceeding 20.4 mm during a snowfall period. Consecutive rise in temperature within three days and daily mean temperature reaching 0.5°C in the following day imply a high probability of temperaturerise-triggered avalanche release. Earthquakes have a significant impact on the formation of large size avalanches in the area. For the period 2011-2017, five cases were identified as a consequence of earthquake with magnitudes of 3.3≤M_L≤5.1 and source-to-site distances of 19~139 km. The Tianshan Mountains are characterized by a continental snow climate with lower snow density, lower snow shear strength and high proportion depth hoar, which explains that both the snowfall and temperature for triggering avalanche release in the continental snow climate of the Tianshan Mountains are lower than that in maritime snow climate and transitional snow climate regions. The findings help forecast avalanche release for mitigating avalanche disaster and assessing the risk of avalanche disaster. 展开更多
关键词 触发因素 雪崩 西方 特征 道路安全 气候分类 中国 地震数据
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Reference evapotranspiration concentration and its relationship with precipitation concentration at southern and northern slopes of Tianshan Mountains, China 被引量:1
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作者 huang fa-rong YANG Tao +3 位作者 LI Qian LI Si-si LI Lan-hai Suwannee ADSAVAKULCHAI 《Journal of Mountain Science》 SCIE CSCD 2019年第6期1381-1395,共15页
The investigation of concentration characteristics of reference evapotranspiration(ETref) is important for water resources management. The concentration index(CI), concentration degree(CD) and concentration period(CP)... The investigation of concentration characteristics of reference evapotranspiration(ETref) is important for water resources management. The concentration index(CI), concentration degree(CD) and concentration period(CP) are used to investigate the concentration characteristics of ETref and the relationship between ETref concentration and precipitation concentration at sub-monthly timescale based on the daily climatic variables from 1966 to 2015 in 27 meteorological stations at the southern and northern slopes of Tianshan Mountains in China. It was found that the CI of ETref is about 0.40 and less concentrated than precipitation in the study area. At the southern slope, the maximum ETref appears in late June and is earlier than the maximum precipitation(early July), ETref distributes more equally than precipitation, and the CI, CD and CP of these two variables do not show significant change based on the Mann–Kendall test. At the northern slope, both the maximum ETref and precipitation appear in early July, and ETref is more dispersed than precipitation. During the study period, the maximum ETref at the northern slope tends to appear earlier due to the impacts of wind speed, relative humidity, sunshine duration, and air temperature. ETref concentration does not match the precipitation concentration in the study area, particularly at the southern slope. The mismatch between ETref and precipitation concentration within a year reveals the water resources pressure on environmental, social and economic sustainability in the study area. 展开更多
关键词 CONCENTRATION Reference EVAPOTRANSPIRATION Precipitation Trend analysis TIANSHAN Mountains
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巩乃斯河谷地带地表土壤水分和电导率的分布特征 被引量:3
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作者 冯挺 黄法融 +1 位作者 郝建盛 李兰海 《干旱区研究》 CSCD 北大核心 2020年第6期1457-1468,共12页
土壤水分和土壤电导率是影响植被生长和农业发展的重要因素,传统方法测量土壤水分和土壤电导率成本高,导致当前缺少基于实测资料的这两种土壤变量在山区流域不同空间尺度下的研究。本研究利用地表土壤水分和电导率实测数据,应用统计学方... 土壤水分和土壤电导率是影响植被生长和农业发展的重要因素,传统方法测量土壤水分和土壤电导率成本高,导致当前缺少基于实测资料的这两种土壤变量在山区流域不同空间尺度下的研究。本研究利用地表土壤水分和电导率实测数据,应用统计学方法,分析了天山西部巩乃斯河谷地带不同空间尺度下秋季地表土壤水分和地表土壤电导率的分布特征及其影响因素。结果表明:(1)在巩乃斯河谷,流域尺度地表土壤水分随海拔的升高而显著(P<0.01)增加,增加速率为每公里10%,但在阿拉图拜小流域,地表土壤水分随海拔的升高先上升后降低;流域尺度平均地表土壤电导率为17.51 mS·m^(-1),表层土壤整体上不存在盐碱化,但2000~2500 m海拔范围内部分点的电导率大于35 mS·m^(-1),为轻度盐渍化;坡地尺度下,不同坡向地表土壤水分和电导率均存在较大差异,阴坡地表土壤水分(均值:44.22%)>阳坡(均值:22.83%),阳坡地表土壤电导率(均值:8.33 mS·m^(-1))>阴坡(均值:4.58 mS·m^(-1));(2)随空间尺度增大,影响土壤特性的环境要素更加复杂,地表土壤水分与地表土壤电导率关系逐渐变弱;(3)不同土地利用类型的地表土壤水分依次为:草地(均值37.19%)>耕地(均值37.04%)>林地(均值34.67%),地表土壤电导率依次为:耕地(均值17.36 mS·m^(-1))>草地(均值14.95 mS·m^(-1))>林地(均值13.81 mS·m^(-1))。在海拔、坡向、土地利用类型的影响下,巩乃斯河谷地带地表土壤电导率和土壤水分均呈中度变异。本研究有益于巩乃斯河流域水土资源合理利用及生态环境保护。 展开更多
关键词 地表土壤水分 地表土壤电导率 空间分布 巩乃斯河流域
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