Continuous measurements in soil and air at the permafrost long-term observatory at the Bayelva station near Ny-Ålesund (2018 et seq) ...

Understanding permafrost processes and changes requires long-term observational datasets of ground and climate variables. Despite the fact that the Arctic climate changes more rapidly than the rest of the globe, observational data density in the region is low and most time series are short. Long ter...

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Bibliographic Details
Published in:Nauchnyi dialog
Main Authors: Boike, Julia, Grünberg, Inge, Miesner, Frederieke, Bornemann, Niko, Cable, William L
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2022
Subjects:
active layer
air temperature
Arctic
Bayelva
dielectricity
dielectric number
Electrical conductivity
Permafrost
precipitation
radiation
relative humidity
relative permittivity
snow depth
snow height
Soil
Soil Moisture
soil temperature
Svalbard
Temperature
water content
wind direction
wind speed
Monitoring station
Permafrost Research AWI_Perma
Ny-Ålesund
Ny Ålesund
permafrost
Online Access:https://dx.doi.org/10.1594/pangaea.948951
https://doi.pangaea.de/10.1594/PANGAEA.948951
Description
Summary:Understanding permafrost processes and changes requires long-term observational datasets of ground and climate variables. Despite the fact that the Arctic climate changes more rapidly than the rest of the globe, observational data density in the region is low and most time series are short. Long term observations are available from the Bayelva Site at Ny-Ålesund, Svalbard, where meteorology, energy balance components and subsurface observations have been made since 1998 and are still continued today. The climate observations include snow depth, snow dielectric number, snow temperature, liquid precipitation, air temperature, relative humidity, wind speed and direction, and radiation fluxes. The below-ground observations cover active layer and permafrost temperature, soil volumetric water content and soil bulk electrical conductivity. Since the data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as snow depth and soil moisture content, ... : ** PLEASE NOTE **If you use these datasets, please cite the publication given in "References".--When clicking on "Download ZIP file containing all datasets" you will only download meteorological data. The soil data needs to be downloaded seperately, download links are available in the zip in file "summary.txt". ...

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