Magnaprobe Snow Depths for the 2019 SALVO Campaign

Delamere, Jennifer; Pinzner, Anika; Sturm, Matthew

doi:10.5439/1962422

Title: Magnaprobe Snow Depths for the 2019 SALVO Campaign

Dataset
Other Related Research

Abstract

The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.

Authors:

;

ORNL

Publication Date:: Tue Mar 21 04:00:00 UTC 2023

Other Number(s):: ARM0717

DOE Contract Number:: AC05-00OR22725

Research Org.:: Atmospheric Radiation Measurement (ARM) Archive, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (US); ARM Data Center, Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Org.:: USDOE Office of Science (SC), Biological and Environmental Research (BER)

Collaborations:: PNNL, BNL, ANL, ORNL

Subject:: 54 ENVIRONMENTAL SCIENCES; Snow Depth

OSTI Identifier:: 1962422

DOI:: https://doi.org/10.5439/1962422

Citation Formats


                    Delamere, Jennifer, Pinzner, Anika, and Sturm, Matthew. Magnaprobe Snow Depths for the 2019 SALVO Campaign.  United States: N. p., 2023. 
        Web.  doi:10.5439/1962422.

Copy to clipboard


                    Delamere, Jennifer, Pinzner, Anika, & Sturm, Matthew. Magnaprobe Snow Depths for the 2019 SALVO Campaign.  United States.  doi:https://doi.org/10.5439/1962422

Copy to clipboard


                    Delamere, Jennifer, Pinzner, Anika, and Sturm, Matthew. 2023.  
"Magnaprobe Snow Depths for the 2019 SALVO Campaign".  United States.  doi:https://doi.org/10.5439/1962422.  https://www.osti.gov/servlets/purl/1962422. Pub date:Tue Mar 21 04:00:00 UTC 2023

Copy to clipboard


                    
@article{osti_1962422,

  title        = {Magnaprobe Snow Depths for the 2019 SALVO Campaign},

  author       = {Delamere, Jennifer and Pinzner, Anika and Sturm, Matthew},

  abstractNote = {The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.},

  doi          = {10.5439/1962422},

  journal      = {},

  number       = ,

  volume       = ,

  place        = {United States},

  year         = {Tue Mar 21 04:00:00 UTC 2023},

  month        = {Tue Mar 21 04:00:00 UTC 2023}

}

Copy to clipboard

Dataset:

View Dataset

DOI: https://doi.org/10.5439/1962422

Save / Share:

Export Metadata

Save to My Library

Similar records in DOE Data Explorer and OSTI.GOV collections:

Magnaprobe Snow Depths for the 2022 SALVO Campaign

Dataset Delamere, Jennifer ; Pinzner, Anika ; Sturm, Matthew

The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.
Snow-substrate interface temperature and air temperature for the SALVO 2019 Campaign

Dataset Pinzner, Anika ; Delamere, Jennifer ; Sturm, Matthew

The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.
Spectral Albedo for the 2019 SALVO Campaign

Dataset Delamere, Jennifer ; Pinzner, Anika ; Sturm, Matthew ; ...

The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.
Snow ALbedo eVOlution (SALVO) Campaign Snow Depth and Related Surface Properties from April - June, 2024 in Utqiagivk, AK

Dataset Oggier, Marc ; Clemens, David ; Espinosa, Zac ; ...

Detailed transects of snow depths and related measurements were made with a magnaprobe along fixed lines in Utqiagvik, AK. The operator measures snow depth by plunging a rod with a sliding basket into the snow and pressing a trigger. At this point, the data logger records the distance between the tip of the rod and the height of the basket, the measurement number, the time, and the geographic location of the measurement. To measure snow depth, the rod tip must be placed at the snow-ground or snow-sea ice interface. The interface can be hard or soft; in the latter case,more »« less
Snow-substrate interface temperature and air temperature for the SALVO 2022 Campaign

Dataset Pinzner, Anika ; Delamere, Jennifer ; Sturm, Matthew ; ...

The springtime, surface-albedo transition in the Alaskan Arctic and the forcings that determine the duration and nature of that transition are the focus of our Snow ALbedo eVOlution (SALVO I & II) campaign. The SALVO team are assessing the “whys” and “how longs” of the stages of the spring melt during which albedo values drop from 0.8 to 0.1, the largest and most significant change of the year. The near-shore location of the ARM NSA observatory makes this an ideal place to investigate these melt stages.

Similar Records