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Spatially distributed water-balance and meteorological data from the rain–snow transition, southern Sierra Nevada, California

机译:加利福尼亚内华达州南部雨雪过渡的空间分布水平衡和气象数据

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We strategically placed spatially distributed sensors to provide representative measures of changes in snowpack and subsurface water storage, plus the fluxes affecting these stores, in a set of nested headwater catchments. The high temporal frequency and distributed coverage make the resulting data appropriate for process studies of snow accumulation and melt, infiltration, evapotranspiration, catchment water balance, (bio)geochemistry, and other critical-zone processes. We present 8?years of hourly snow-depth, soil-moisture, and soil-temperature data, as well as 14?years of quarter-hourly streamflow and meteorological data that detail water-balance processes at Providence Creek, the upper part of which is at the current 50?% rain versus snow transition of the southern Sierra Nevada, California. Providence Creek is the long-term study cooperatively run by the Southern Sierra Critical Zone Observatory (SSCZO) and the USDA Forest Service Pacific Southwest Research Station's Kings River Experimental Watersheds (KREW). The 4.6?km sup2/sup montane Providence Creek catchment spans the current lower rain–snow transition elevation of 1500–2100?m. Two meteorological stations bracket the high and low elevations of the catchment, measuring air temperature, relative humidity, solar radiation, precipitation, wind speed and direction, and snow depth, and at the higher station, snow water equivalent. Paired flumes at three subcatchments and a V-notch weir at the integrating catchment measure quarter-hourly streamflow. Measurements of meteorological and streamflow data began in 2002. Between 2008 and 2010, 50 sensor nodes were added to measure distributed snow depth, air temperature, soil temperature, and soil moisture within the top 1?m below the surface. These sensor nodes were installed to capture the lateral differences of aspect and canopy coverage. Data are available at hourly and daily intervals by water year (1?October–30?September) in nonproprietary formats from online data repositories.
机译:我们策略性地放置了空间分布的传感器,以提供一组嵌套水源集水区中积雪和地下蓄水量变化的典型测量值,以及影响这些蓄水量的通量。较高的时间频率和分布的覆盖范围使所得的数据适合于积雪和融雪,入渗,蒸散,集水区水平衡,(生物)地球化学和其他关键区域过程的过程研究。我们提供了8年的每小时降雪深度,土壤湿度和土壤温度数据,以及14小时的每季度每小时流量和气象数据,这些数据详细描述了Providence Creek的水平衡过程,其上部目前加利福尼亚内华达山脉南部的降雨与降雪量之间的比例为50%。普罗维登斯溪(Providence Creek)是由南部山脉关键地区天文台(SSCZO)和美国农业部森林服务局太平洋西南研究站的金斯河实验流域(KREW)合作开展的一项长期研究。 4.6?km的 2 山地普罗维登斯溪流域跨越了目前较低的雨雪过渡高度1500-2100?m。两个气象站分别对流域的高低海拔进行测量,以测量空气温度,相对湿度,太阳辐射,降水,风速和风向以及积雪深度,而在较高的气象站则测量雪水当量。在三个子汇水区的成对水槽和在综合集水区的V型槽堰测量每季度每小时流量。气象和流量数据的测量始于2002年。在2008年至2010年之间,添加了50个传感器节点,以测量地表以下1?m内的分布雪深,气温,土壤温度和土壤湿度。安装这些传感器节点是为了捕获外观和顶篷覆盖范围的横向差异。可以从水数据年(每小时1月至10月30日至9月)按小时和每天的间隔以非专有格式从在线数据存储库中获取数据。

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