Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs

A majority of the annual precipitation in many mountains falls as snow, and obtaining accurate estimates of the amount of water stored within the snowpack is important for water supply forecasting. Mountain topography can produce complex patterns of snow distribution, accumulation, and ablation, yet...

Full description

Bibliographic Details
Main Authors: Douglas M. Hultstrand, Steven R. Fassnacht, John D. Stednick, Christopher A. Hiemstra
Format: Article
Language:English
Published: MDPI AG 2021-12-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/13/1/3
_version_ 1797495969099546624
author Douglas M. Hultstrand
Steven R. Fassnacht
John D. Stednick
Christopher A. Hiemstra
author_facet Douglas M. Hultstrand
Steven R. Fassnacht
John D. Stednick
Christopher A. Hiemstra
author_sort Douglas M. Hultstrand
collection DOAJ
description A majority of the annual precipitation in many mountains falls as snow, and obtaining accurate estimates of the amount of water stored within the snowpack is important for water supply forecasting. Mountain topography can produce complex patterns of snow distribution, accumulation, and ablation, yet the interaction of topography and meteorological patterns tends to generate similar inter-annual snow depth distribution patterns. Here, we question whether snow depth patterns at or near peak accumulation are repeatable for a 10-year time frame and whether years with limited snow depth measurement can still be used to accurately represent snow depth and mean snow depth. We used snow depth measurements from the West Glacier Lake watershed, Wyoming, USA, to investigate the distribution of snow depth. West Glacier Lake is a small (0.61 km<sup>2</sup>) windswept (mean of 8 m/s) watershed that ranges between 3277 m and 3493 m. Three interpolation methods were compared: (1) a binary regression tree, (2) multiple linear regression, and (3) generalized additive models. Generalized additive models using topographic parameters with measured snow depth presented the best estimates of the snow depth distribution and the basin mean amounts. The snow depth patterns near peak accumulation were found to be consistent inter-annually with an average annual correlation coefficient (r<sup>2</sup>) of 0.83, and scalable based on a winter season accumulation index (r<sup>2</sup> = 0.75) based on the correlation between mean snow depth measurements to Brooklyn Lake snow telemetry (SNOTEL) snow depth data.
first_indexed 2024-03-10T01:57:00Z
format Article
id doaj.art-944e80de364349368aae0e7e580bfe62
institution Directory Open Access Journal
issn 2073-4433
language English
last_indexed 2024-03-10T01:57:00Z
publishDate 2021-12-01
publisher MDPI AG
record_format Article
series Atmosphere
spelling doaj.art-944e80de364349368aae0e7e580bfe622023-11-23T12:55:31ZengMDPI AGAtmosphere2073-44332021-12-01131310.3390/atmos13010003Snowpack Distribution Using Topographical, Climatological and Winter Season Index InputsDouglas M. Hultstrand0Steven R. Fassnacht1John D. Stednick2Christopher A. Hiemstra3EASC-Watershed Science, Colorado State University, Fort Collins, CO 80523-1482, USAESS-Watershed Science, Colorado State University, Fort Collins, CO 80523-1476, USAFRS-Watershed Science, College of Natural Resources, Colorado State University, Fort Collins, CO 80523-1872, USAUSDA Forest Service, Geospatial Management Office, Salt Lake City, UT 84138-1101, USAA majority of the annual precipitation in many mountains falls as snow, and obtaining accurate estimates of the amount of water stored within the snowpack is important for water supply forecasting. Mountain topography can produce complex patterns of snow distribution, accumulation, and ablation, yet the interaction of topography and meteorological patterns tends to generate similar inter-annual snow depth distribution patterns. Here, we question whether snow depth patterns at or near peak accumulation are repeatable for a 10-year time frame and whether years with limited snow depth measurement can still be used to accurately represent snow depth and mean snow depth. We used snow depth measurements from the West Glacier Lake watershed, Wyoming, USA, to investigate the distribution of snow depth. West Glacier Lake is a small (0.61 km<sup>2</sup>) windswept (mean of 8 m/s) watershed that ranges between 3277 m and 3493 m. Three interpolation methods were compared: (1) a binary regression tree, (2) multiple linear regression, and (3) generalized additive models. Generalized additive models using topographic parameters with measured snow depth presented the best estimates of the snow depth distribution and the basin mean amounts. The snow depth patterns near peak accumulation were found to be consistent inter-annually with an average annual correlation coefficient (r<sup>2</sup>) of 0.83, and scalable based on a winter season accumulation index (r<sup>2</sup> = 0.75) based on the correlation between mean snow depth measurements to Brooklyn Lake snow telemetry (SNOTEL) snow depth data.https://www.mdpi.com/2073-4433/13/1/3snow depthwinter season indexuncertaintysnow water equivalentmodelingfun in the snow
spellingShingle Douglas M. Hultstrand
Steven R. Fassnacht
John D. Stednick
Christopher A. Hiemstra
Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
Atmosphere
snow depth
winter season index
uncertainty
snow water equivalent
modeling
fun in the snow
title Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
title_full Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
title_fullStr Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
title_full_unstemmed Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
title_short Snowpack Distribution Using Topographical, Climatological and Winter Season Index Inputs
title_sort snowpack distribution using topographical climatological and winter season index inputs
topic snow depth
winter season index
uncertainty
snow water equivalent
modeling
fun in the snow
url https://www.mdpi.com/2073-4433/13/1/3
work_keys_str_mv AT douglasmhultstrand snowpackdistributionusingtopographicalclimatologicalandwinterseasonindexinputs
AT stevenrfassnacht snowpackdistributionusingtopographicalclimatologicalandwinterseasonindexinputs
AT johndstednick snowpackdistributionusingtopographicalclimatologicalandwinterseasonindexinputs
AT christopherahiemstra snowpackdistributionusingtopographicalclimatologicalandwinterseasonindexinputs