近36年藏东“三江”流域农业气候资源变化特征

为了解藏东"三江"流域农业气候资源的变化特征,为政府部门合理利用气候资源提供科学依据。利用藏东"三江"流域1980—2015年逐日气温、降水量、日照时数等资料,应用线性倾向估计、M-K突变检验等方法,分析近36年藏东"三江"流域热量、光照、降水资源的变化趋势及对农业生产的影响。结果表明:近36年,藏东"三江"流域年平均气温、日照时数、降水量呈增加趋势,气候倾向率分别为0.38℃/10 a、22.2 h/10 a、9.4 mm/10 a;流域内各站气温年、季变化趋势一致,日照时数与降水量年、季变化趋势差异较大;降水相对变率春季最大,夏季最小;≥0℃的初日提早、终日推迟,持续日数延长,积温增长。农业气候资源的变化将对藏东"三江"流域农业的发展产生巨大影响。     

新一代温室气体排放情景下安徽省未来气候变化预估分析

基于联合国政府间气候变化专门委员会(IPCC)发布的新一代排放情景,和中国气象局发布的"中国地区气候变化预估数据集V3.0",针对安徽省,笔者选择1971—2000年作为基准期,采用区域气候模式模拟的方法,对比分析安徽省未来气候变化特征,重点评估近期内即未来20年气候变化趋势。模拟结果显示,未来20年不同情景下安徽省平均气温均为上升,全省平均增温幅度约0.9~1.1℃;而降水量变化具有不同特征,较低排放情景下降水量以上升为主,高排放情景则以下降为主。到2050s全省平均气温相比于基准期将升高1.6~1.7℃,升温幅度呈现北高南低的特征;全省降水量相比于基准期将下降50~90 mm,各地降水量均呈下降趋势。另外,通过对降水和气温的模拟,预估未来该地区旱涝演替更加频繁,高温热浪等事件也将进一步频发。     

基于GIS和气候-土地利用信息的西藏青稞种植适宜性区划

使用2009—2013年的CLDAS大气驱动场(V1.0)数据为气候数据源,结合影响西藏青稞种植的关键气候因子,确定生育期≥0℃的积温(T0)、最热月平均气温(Tmax)、生育期降水量(R)这3个气候因子作为西藏青稞种植区划指标,利用GIS技术进行西藏青稞种植气候适应性区划。为了得到既能满足气候需求又有耕地的实际可种植区域,本研究将土地资源信息与气候区划叠加。结果表明:青稞最适宜种植区域主要分布于雅江中游河谷2400~4100 m区域及昌都市的中部和南部,结果与事实相符。     

青藏高原草地降水利用效率时空动态及对气候变化的响应

本研究利用CASA(Carnegie-Ames-Stanford Approach)模型模拟了2000—2013年青藏高原草地净植被生产力(Net Primary Production,NPP),结合实测数据、气象数据和土地覆被数据计算了草地降水利用效率（PUE）,探究其时空分布特征,以及不同草地类型PUE及其对气候变化的响应。结果表明：青藏高原草地PUE在研究年限内呈现波动增加趋势,增加速率为每年0.0035 g·m^-2·mm^-1,14 a的平均值为0.38 g·m^-2·mm^-1。PUE的空间分布具有明显的异质性,呈现东部高、中西部低的基本格局。PUE分布在0.2～0.4 g·m^-2·mm^-1之间的比例最大,占青藏高原总面积的55.63%,呈减少趋势的区域主要分布在青藏高原的北部和西部,以及东部的边界地区,呈增加趋势的地区集中在研究区的中部和南部。研究年限内PUE的变异系数分布在0.07～0.85之间,变化稳定的区域所占面积最大,为总面积的43.43%,主要分布在唐古拉山脉和横断山脉附近。不同草地类型间PUE均值存在差异,具体表现为：草甸（1.06 g·m^-2·mm^-1）>坡面草地（0.80 g·m^-2·mm^-1）>平原草地（0.30 g·m^-2·mm^-1）>高山与亚高山草甸（0.29 g·m^-2·mm^-1）>荒漠草地（0.23 g·m^-2·mm^-1）>高山与亚高山草地（0.094 g·m^-2·mm^-1）。总体上,青藏高原草地PUE与降水成负相关关系,而与气温呈正相关,PUE的变化对降水响应更加敏感。     

Tomato brown rugose fruit disease: current distribution,knowledge and future prospects

Tomato is the most economically important fruit/vegetable crop grown worldwide. However, viral diseases remain an important factor limiting its productivity, with estimated quantitative and qualitative yield losses in tomato crops often reaching up to 100%. Many viruses infecting tomato have been reported, while new viral diseases have also emerged. The climatic changes the world is experiencing can be a contributing factor to the successful spread of newly emerging viruses, as well as the establishment of disease in areas that were previously either unfavourable or where the disease was absent. Because antiviral products are not available, strategies to mitigate viral diseases rely on genetic resistance/tolerance to infection, control of vectors, improvement in crop hygiene, roguing of infected plants and seed certification. Tomato brown rugose fruit virus (ToBRFV) is an emerging viral threat to tomato productivity and is currently spreading into new areas, which is of great concern to the growing global production in the absence of mitigation measures. This review presents the current knowledge about ToBRFV and future prospects for an improved understanding of the virus, which will be needed to support effective control and mitigation of the impact it is likely to cause.     

1957—2015年叶尔羌河流域气候变化特征及其径流响应

根据流域内气象、水文站点的长期观测数据,利用线性趋势、相关系数、累积距平、Mann-kendall(M-K)突变检验等方法分析不同区域的干、湿季气候变化特征,并假定不同的气候情景组合,分析径流对气候变化的响应程度。结果表明:(1)1957-2015年4个单元气温和降水量呈增加趋势;除上游外,相对湿度、平均风速和大风日数呈减小趋势,流域径流量呈增加趋势。(2)气温在1996年发生突变;降水量未出现明显突变点;相对湿度在2005年左右发生突变;除下游外,平均风速在1983年发生突变;径流量于1993年发生突变,突变后径流量增加了9.08×10^8m^3。(3)相关性分析显示,流域径流量与湿季平均气温、平均最低(最高)气温呈极显著正相关,与湿季平均风速、大风日数和相对湿度呈负相关,除上游径流与干季降水量呈正相关外,其他区域与降水量呈负相关。(4)敏感性分析表明,当降水量不变,气温升高1℃,径流量增加9.06%;当气温不变,降水量增加10%,径流量减小1.67%,这主要与径流组成有关。流域77.4%的径流量来自雪冰融水补给,当降水量增加时,气温降低,减少了冰川积雪的融化,因而流域径流与气温呈正相关,与降水量呈负相关,且对气温变化更敏感。     

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.