2022
DOI: 10.1002/ecs2.4094
|View full text |Cite|
|
Sign up to set email alerts
|

Collaborative wildlife–snow science: Integrating wildlife and snow expertise to improve research and management

Abstract: For wildlife inhabiting snowy environments, snow properties such as onset date, depth, strength, and distribution can influence many aspects of ecology, including movement, community dynamics, energy expenditure, and forage accessibility. As a result, snow plays a considerable role in individual fitness and ultimately population dynamics, and its evaluation is, therefore, important for comprehensive understanding of ecosystem processes in regions experiencing snow. Such understanding, and particularly study of… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
11
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6

Relationship

1
5

Authors

Journals

citations
Cited by 12 publications
(11 citation statements)
references
References 152 publications
0
11
0
Order By: Relevance
“…SWE is the vertical depth of water that would be produced if the snow was instantaneously melted on a horizontal surface (USDA, 2022). Thus, in the absence of actual snow depth, we presented SWE depth (in centimeters) based on a unit conversion (1 kg/m 2 = 0.1 cm) to aid interpretation (Reinking et al, 2022). However, if spatial snow densities (ρs$$ {\uprho}_s $$) were available, we could translate estimates of SWE depth to snow depth (HS) via the following equation: SWEgoodbreak=HSgoodbreak×normalρsnormalρw,$$ \mathrm{SWE}=\mathrm{HS}\times \frac{\uprho_s}{\uprho_w}, $$ where ρw$$ {\uprho}_w $$ is the density of water (Reinking et al, 2022).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…SWE is the vertical depth of water that would be produced if the snow was instantaneously melted on a horizontal surface (USDA, 2022). Thus, in the absence of actual snow depth, we presented SWE depth (in centimeters) based on a unit conversion (1 kg/m 2 = 0.1 cm) to aid interpretation (Reinking et al, 2022). However, if spatial snow densities (ρs$$ {\uprho}_s $$) were available, we could translate estimates of SWE depth to snow depth (HS) via the following equation: SWEgoodbreak=HSgoodbreak×normalρsnormalρw,$$ \mathrm{SWE}=\mathrm{HS}\times \frac{\uprho_s}{\uprho_w}, $$ where ρw$$ {\uprho}_w $$ is the density of water (Reinking et al, 2022).…”
Section: Methodsmentioning
confidence: 99%
“…Thus, in the absence of actual snow depth, we presented SWE depth (in centimeters) based on a unit conversion (1 kg/m 2 = 0.1 cm) to aid interpretation (Reinking et al, 2022). However, if spatial snow densities (ρs$$ {\uprho}_s $$) were available, we could translate estimates of SWE depth to snow depth (HS) via the following equation: SWEgoodbreak=HSgoodbreak×normalρsnormalρw,$$ \mathrm{SWE}=\mathrm{HS}\times \frac{\uprho_s}{\uprho_w}, $$ where ρw$$ {\uprho}_w $$ is the density of water (Reinking et al, 2022). In our study area, average snowpack densities were only available at a single location each year, so we relied on SWE depth and used the R packages daymetr (Hufkens et al, 2018) and FedData (Bocinsky, 2019) to mosaic the daily tiles.…”
Section: Methodsmentioning
confidence: 99%
“…Fine‐scale snow data could be useful in many wildlife studies (Boelman et al 2019, Reinking et al 2022). Remotely sensed, satellite‐based, and modelled snow data products are coarse scale (typically hundreds of meters to several kilometers), frequently prone to error in complex forested terrain (Sirén et al 2018), and do not capture the considerable spatial variability of snow depth under forest canopies (Jost et al 2007).…”
Section: Figurementioning
confidence: 99%
“…Fine-scale snow data could be useful in many wildlife studies (Boelman et al 2019, Reinking et al 2022.…”
mentioning
confidence: 99%
“…Seasonal snow cover shapes a suite of ecological processes across nearly half of all land in the Northern Hemisphere (Robinson et al 2014, Niittynen et al 2018). The dynamic nature of snow throughout the landscape and throughout the year presents a challenge Defining the danger zone: critical snow properties for predatorprey interactions for evaluating wildlife-snow relationships (Reinking et al 2022). Furthermore, climate change is rapidly altering seasonal snowpacks globally, with the greatest effects observed across northern Eurasia and North America (IPCC 2022).…”
Section: Introductionmentioning
confidence: 99%