Soil data at station Samoylov (2019)

Fuente: PANGAEA
Saved in:
Bibliographic Details
Main Authors: Boike, Julia, Bolshiyanov, Dimitry Yu, Bornemann, Niko, Grigoriev, Mikhail N, Grünberg, Inge, Lange, Stephan, Miesner, Frederieke
Format: Dataset Open Access
Language:en
Published: PANGAEA 2022
Subjects:
Online Access:
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1867171316461731840
author Boike, Julia
Bolshiyanov, Dimitry Yu
Bornemann, Niko
Grigoriev, Mikhail N
Grünberg, Inge
Lange, Stephan
Miesner, Frederieke
author_facet Boike, Julia
Bolshiyanov, Dimitry Yu
Bornemann, Niko
Grigoriev, Mikhail N
Grünberg, Inge
Lange, Stephan
Miesner, Frederieke
collection Datos científicos de ciencias marinas y ambientales
contents Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term observational site Samoylov, located in the Lena River Delta, Siberia (72.37°N, 126.48°E). The location is characterized by a cold, dry tundra climate with mean annual air temperature of -11.7°C (using years with complete data between 1998 and 2017). The monthly mean temperatures over this period varied between 9.4°C in the warmest month (July) and -31.7°C in the coldest month (February). The average summer rainfall (June-October) was 145.2 mm. This dataset adds recent years to the observations of meteorological parameters, energy balance, and subsurface observations which have been recorded since 1998. The instrumentation, calibration, processing and data quality control is explained in Boike et al. (2019). The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as ground heat flux, active layer and permafrost temperature, soil volumetric water content, relative permittivity, and soil bulk electrical conductivity. Those variables were measured at various depths and beneath different microtopographic features (a polygon center, a rim, a slope, and a trough), representing landscape heterogeneity. The observations are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_947034
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Soil data at station Samoylov (2019)
Boike, Julia
Bolshiyanov, Dimitry Yu
Bornemann, Niko
Grigoriev, Mikhail N
Grünberg, Inge
Lange, Stephan
Miesner, Frederieke
AWI_Perma; dataset; LTO; LTO_Permafrost_Samoylov; Permafrost Research; Samoylov; Samoylov_WST; Samoylov Island, Lena Delta, Siberia; Samoylov permafrost long-term observations; Soil; Weather station/meteorological observation; WST
Understanding permafrost processes and changes requires long-term observational datasets. This dataset is a continuation of the dataset available from the long-term observational site Samoylov, located in the Lena River Delta, Siberia (72.37°N, 126.48°E). The location is characterized by a cold, dry tundra climate with mean annual air temperature of -11.7°C (using years with complete data between 1998 and 2017). The monthly mean temperatures over this period varied between 9.4°C in the warmest month (July) and -31.7°C in the coldest month (February). The average summer rainfall (June-October) was 145.2 mm. This dataset adds recent years to the observations of meteorological parameters, energy balance, and subsurface observations which have been recorded since 1998. The instrumentation, calibration, processing and data quality control is explained in Boike et al. (2019). The data provide observations of temporally variable parameters that mitigate energy fluxes between permafrost and atmosphere, such as ground heat flux, active layer and permafrost temperature, soil volumetric water content, relative permittivity, and soil bulk electrical conductivity. Those variables were measured at various depths and beneath different microtopographic features (a polygon center, a rim, a slope, and a trough), representing landscape heterogeneity. The observations are suitable for use in integrating, calibrating and testing permafrost as a component in Earth System Models. The resulting quality-controlled dataset is unique in the Arctic and serves as a baseline for future studies.
title Soil data at station Samoylov (2019)
topic AWI_Perma; dataset; LTO; LTO_Permafrost_Samoylov; Permafrost Research; Samoylov; Samoylov_WST; Samoylov Island, Lena Delta, Siberia; Samoylov permafrost long-term observations; Soil; Weather station/meteorological observation; WST
url https://doi.org/10.1594/PANGAEA.947034