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Obtaining sub-daily new snow density from automated measurements in high mountain regions

机译:从高山地区自动测量获得次日新雪密度

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The density of new snow is operationally monitored by meteorological or hydrological services at daily time intervals, or occasionally measured in local field studies. However, meteorological conditions and thus settling of the freshly deposited snow rapidly alter the new snow density until measurement. Physically based snow models and nowcasting applications make use of hourly weather data to determine the water equivalent of the snowfall and snow depth. In previous studies, a number of empirical parameterizations were developed to approximate the new snow density by meteorological parameters. These parameterizations are largely based on new snow measurements derived from local in situ measurements. In this study a data set of automated snow measurements at four stations located in the European Alps is analysed for several winter seasons. Hourly new snow densities are calculated from the height of new snow and the water equivalent of snowfall. Considering the settling of the new snow and the old snowpack, the average hourly new snow density is 68 kg m(-3), with a standard deviation of 9 kg m(-3). Seven existing parameterizations for estimating new snow densities were tested against these data, and most calculations overestimate the hourly automated measurements. Two of the tested parameterizations were capable of simulating low new snow densities observed at sheltered inner-alpine stations. The observed variability in new snow density from the automated measurements could not be described with satisfactory statistical significance by any of the investigated parameterizations. Applying simple linear regressions between new snow density and wet bulb temperature based on the measurements' data resulted in significant relationships (r(2) 0.5 and p = 0.05) for single periods at individual stations only. Higher new snow density was calculated for the highest elevated and most wind-exposed station location. Whereas snow measurements using ultrasonic devices and s
机译:新雪的密度由日常时间间隔的气象或水文服务进行操作,或者在当地研究中偶尔测量。然而,气象条件并因此稳定新沉积的雪迅速改变新的雪密度直至测量。物理基础的雪模型和现在播放应用程序利用每小时天气数据来确定降雪和雪深的水。在以前的研究中,开发了许多经验参数来通过气象参数近似新的雪密度。这些参数化主要基于从局部源于原位测量的新雪测量。在这项研究中,分析了位于欧洲阿尔卑斯山的四个站的自动雪测量数据集进行了几个冬季。每小时新的雪密度都是从新雪的高度和降雪量的高度计算的。考虑到新雪和旧积雪的沉降,平均每小时新的雪密度为68千克(-3),标准偏差为9千克M(-3)。针对这些数据测试了七个用于估计新雪密度的参数化,大多数计算估计每小时自动测量。两种测试的参数化能够模拟在庇护内高山站观察到的低新雪密度。通过任何调查的参数化,无法描述从自动测量中的新雪密度的观察到的可变性,任何调查的参数都无法达到令人满意的统计学意义。基于测量数据的新雪密度和湿灯泡温度之间的简单线性回归导致仅在单个站的单个时段的显着关系(R(2)& 0.5和P& = 0.05)。为最高升高和大多数风险的站位置计算出较高的新雪密度。虽然使用超声装置和s的雪测量

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