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[PDF] Top 20 Changes in the snow water equivalent in mountainous basins in Slovakia over recent decades

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Changes in the snow water equivalent in mountainous basins in Slovakia over recent decades

Changes in the snow water equivalent in mountainous basins in Slovakia over recent decades

... The parameters of the Hron rainfall-runoff model were cali- brated using the method of genetic algorithms, with the aim of achieving the best agreement between the observed and modelled mean daily discharges at the basin ... See full document

8

Variations in water storage in China over recent decades from GRACE observations and GLDAS

Variations in water storage in China over recent decades from GRACE observations and GLDAS

... integrated changes in the vertical components of TWS, is the difference between current and previous months’ TWS ...the water balance with precipitation, evapotranspiration and runoff data in a specific ... See full document

14

Lake volume and groundwater storage variations in Tibetan Plateau's endorheic basin

Lake volume and groundwater storage variations in Tibetan Plateau's endorheic basin

... quantitative water mass budget in the TP is poorly ...annual changes in lake area, level, and volume during 1970s – ...volume changes during 1970s – 2015: a slight decrease of ...a recent ... See full document

11

Remote Sensing, Model Derived and Ground Measurements of Snow Water Equivalent and Snow Density in Alaska

Remote Sensing, Model Derived and Ground Measurements of Snow Water Equivalent and Snow Density in Alaska

... for snow water pitation gages ce air ...thin snow, high evaporative potential leading to snow-bridging and differential stress on the perimeter during periods of rapid snow settlement ... See full document

10

Snow Water Equivalent Estimation for a Snow Covered Prairie Grass Field by GPS Interferometric Reflectometry

Snow Water Equivalent Estimation for a Snow Covered Prairie Grass Field by GPS Interferometric Reflectometry

... the snow-covered prairie grass field di- ...the snow layer and an elevation angle of 5˚, the first Fresnel zone [44] is calculated to have a major axis length of approximately 36 m and a minor axis length ... See full document

11

A global water resources ensemble of hydrological models: the eartH2Observe Tier-1 dataset

A global water resources ensemble of hydrological models: the eartH2Observe Tier-1 dataset

... The data used to force the models were from the WFDEI dataset (Weedon et al., 2011, 2014) that comprised the pe- riod between and including 1979 and 2012 and contains both 3-hourly time intervals and daily time ... See full document

25

A Comparative Evaluation of Snow Depth and Snow Water Equivalent Using Empirical Algorithms and Multivariate regressions

A Comparative Evaluation of Snow Depth and Snow Water Equivalent Using Empirical Algorithms and Multivariate regressions

... to water resources management, such as investigation on surface water, groundwater, snow and ice, dynamic monitoring of ecology, estimation of water amount necessary for keeping and recovering ... See full document

7

Changes in definition lead to changes in the clinical characteristics across COPD categories according to GOLD 2017: a national cross-sectional survey in China

Changes in definition lead to changes in the clinical characteristics across COPD categories according to GOLD 2017: a national cross-sectional survey in China

... All statistical analyses were performed with SPSS version 17.0 (SPSS, Chicago, IL, USA). Descriptive data with normal distribution were expressed as means ± SD. Descriptive data without normal distribution were expressed ... See full document

8

Modelling the spatial variability of snow water equivalent at the catchment scale

Modelling the spatial variability of snow water equivalent at the catchment scale

... In this study we have assumed identical distributions of stochastic unit fields of accumulation and of melt. Observed spatial fields of snowmelt are scarce but from a research site near Trondheim in central Norway, 4 ... See full document

8

Methods to estimate changes in soil water for phenotyping root activity in the field

Methods to estimate changes in soil water for phenotyping root activity in the field

... soil water content are more similar between different soil types than those between the count of thermalized neutrons and soil water ...soil water content to depth ...soil water at ... See full document

17

Response of the intertropical convergence zone to climate change : location, width and strength

Response of the intertropical convergence zone to climate change : location, width and strength

... The zonal-mean theory for ITCZ location undoubtedly gives insights into why the ITCZ lies north of the equator in today’s climate, and provides a quantitative framework with which to examine past and future ITCZ shifts. ... See full document

16

Changes in insect populations in the field in relation to preceding weather conditions

Changes in insect populations in the field in relation to preceding weather conditions

... north of London, where the trapping was carried out, the rainfall is low, averaging about 27 in. (68 cm.) per year with no month averaging below 1*9 in. or above 2-7 in. The rainfall is, in fact, very evenly distributed ... See full document

27

On the contribution of groundwater storage to interannual streamflow anomalies in the Colorado River basin

On the contribution of groundwater storage to interannual streamflow anomalies in the Colorado River basin

... soil water flux and streamflow, and without an explicit rep- resentation of the water table, the land surface water budget may not close other than on very long time averages (Yeh and Eltahir, ... See full document

17

A regional climate model hindcast for Siberia: analysis of snow water equivalent

A regional climate model hindcast for Siberia: analysis of snow water equivalent

... We use ESA GlobSnow for assessing the skill and added value of CCLM relative to global reanalyses for Siberia be- cause of its more sophisticated approach to retrieve SWE from passive microwave satellite data than given ... See full document

18

Factors affecting safe navigation and their impacts in port area

Factors affecting safe navigation and their impacts in port area

... Maritime freight transport has experienced strong growth and profound changes over recent decades. Freight volumes and container traffic in particular have grown with the intensification of ... See full document

39

Use of satellite derived data for characterization of snow cover and simulation of snowmelt runoff through a distributed physically based model of runoff generation

Use of satellite derived data for characterization of snow cover and simulation of snowmelt runoff through a distributed physically based model of runoff generation

... of snow cover characteristics (SWE, snow depth, snowmelt, ...of snow pack and with the use of satellite measurements of ...calculated snow cover fields and for calibra- tion of the snow ... See full document

12

Modeling bulk density and snow water equivalent using daily snow depth observations

Modeling bulk density and snow water equivalent using daily snow depth observations

... estimates over timescales of days, den- sity variations associated with individual storms and melt events are missing from both the Sturm and Jonas mod- ...between snow depth and density at two separate ... See full document

16

Large scale snow water equivalent status monitoring: comparison of different snow water products in the upper Colorado Basin

Large scale snow water equivalent status monitoring: comparison of different snow water products in the upper Colorado Basin

... the snow density, which was changed from 450 to 320 kg m −3 – a value that is more appropri- ate for the study area (Josberger et ...Sierra Snow Laboratory collected in the winter of 1985– ...has ... See full document

13

LIDAR INVESTIGATIONS OF SNOW DISTRIBUTION IN MOUNTAINOUS TERRAIN

LIDAR INVESTIGATIONS OF SNOW DISTRIBUTION IN MOUNTAINOUS TERRAIN

... Snow-volume estimates can be combined with snow density measurements to estimate snow-water equivalent (SWE). This method should decrease field time and improve the accuracy of basin e[r] ... See full document

74

An assessment of sub-snow GPS for quantification of snow water equivalent

An assessment of sub-snow GPS for quantification of snow water equivalent

... A snow pil- low (Sommer Messtechnik SP3) and a snow scale (Sommer Messtechnik SSG1000) serve as reference data for SWE esti- ...The snow pillow measures the overlying pressure of the snowpack on a ... See full document

15

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