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田璐

作品数:3 被引量:12H指数:2
供职机构:中国农业大学资源与环境学院更多>>
发文基金:国家自然科学基金高等学校科技创新工程重大项目北京市科委项目更多>>
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Temporal and Spatial Characteristics of Rainstorm during the Crops Growth Period in North China Region
2010年
By using the daily precipitation data from 1961 to 2005 in North China region,the temporal and spatial distribution characteristics of rainstorm process occurrence and the rainstorm intensity during the crops growth period were studied.The results showed that the rainstorm intensity and the rainstorm process during the crops growth period in North China region both had the obvious annual fluctuations and era variation characteristics.Although the rainstorm and heavy rainstorm occurred in North China region every year,the annual variations were great,and the variation coefficients respectively reached 36.9% and 53.1%.The torrential rain occurred once in every 4-5 years,and the rainstorm process occurred once in every 11 years.Although the torrential rain and rainstorm process occurred in fewer years,their annual fluctuations were more obvious.The peak value zones of rainstorm intensity which was greater and the rainstorm process which occurred frequently were in the 1960s.After 1999,the rainstorm intensity and the rainstorm process were in low value zone of historical stage from 1961 to 2005.Moreover,the 1970s-1990s was between high value and low value,and the rainstorms in different intensities which weren't synchronous happened in the period.In addition,the spatial distribution of annual average rainstorm days presented the tendency which increased obviously from northwest to southeast in Northern China,and the variation coefficient of rainstorm days presented the tendency which increased gradually from southeast to northwest.Generally,the more the annual average rainstorm days are,the smaller the variation coefficient is,and vice versa.The statistics results also showed that precipitation in North China had obvious positive correlation relationship with the rainstorm days.
叶彩华侯双双姜会飞高静田璐
关键词:RAINSTORMPRECIPITATION
华北地区作物生长期暴雨的时空特征被引量:2
2010年
利用华北地区1961~2005年逐日降水数据资料,统计分析了华北地区作物生长期暴雨强度和暴雨过程发生的时空分布特征。结果表明,华北地区作物生长期暴雨强度和暴雨过程具有明显的年际波动和年代变化特征;华北地区虽然年年都发生暴雨和大暴雨,但年际变化较大,变异系数分别高达36.9%和53.1%;特大暴雨每4~5年发生1次,暴雨过程则平均11年一遇,特大暴雨和暴雨过程虽然只发生在较少的年份,但年际间波动更加明显;20世纪60年代是暴雨强度较大和暴雨过程多发期的峰值区,而1999年以后暴雨强度和暴雨过程则处于1961~2005年历史阶段的低值区;70~90年代则处于两者之间,期间不同强度暴雨发生并不同步。此外,华北地区年均暴雨日数空间分布呈现从西北向东南明显增加的趋势,暴雨日数变异系数则呈现自东南向西北逐渐增大的趋势。一般地,年均暴雨日数越多,变异系数越小,反之亦然。统计还表明,华北地区降水量与暴雨日数之间存在明显的正相关关系。
叶彩华侯双双姜会飞高静田璐
关键词:生长期暴雨暴雨过程降水量
退耕还林还草工程对土地利用/覆被变化及景观格局的影响——以张家口市为例被引量:10
2015年
以张家口市为例,根据1989、2000和2010年3期Landsat TM遥感数据,利用土地利用变化模型,景观指数以及GIS技术,系统分析了土地利用/覆被及其景观格局的变化过程和规律,探讨了退耕还林还草工程对土地利用/覆被变化及其景观格局的影响。结果表明,1989—2010年张家口市土地利用结构由以耕地和草地为主,转变为以林地和草地为主。2000年退耕还林还草工程实施以来,耕地减少幅度增加,动态度指数由-0.27%变为-0.83%,林地增加幅度加大,动态度指数由0.56%变为1.39%,草地在数量上表现为减少。退耕前,耕地主要转为草地,退耕后,耕地主要转为林地,耕地转为林地的比例由退耕前的22.50%增加为退耕后的45.46%,退耕后684.85km2的草地转为林地。期间,研究区景观格局趋向均衡化,景观多样性降低,景观破碎化程度上升,景观形状趋于简单。这主要是由于经济建设等人类活动对土地利用和景观格局的干扰程度变大所致。
田璐许月卿孙丕苓
关键词:退耕还林还草
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