iffylaw/PIC: Permafrost Indices Computing

An R package permafrost indices computing (PIC) was developed, which integrates meteorological observations, remote sensing data, and field measurements to compute the factors or indices of permafrost and seasonal frozen soil. At present, 16 temperature/depth-related indices are integrated into the...

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Main Author: Lihui Luo
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2018
Subjects:
Online Access:https://doi.org/10.5281/zenodo.1220663
id ftzenodo:oai:zenodo.org:1220663
record_format openpolar
spelling ftzenodo:oai:zenodo.org:1220663 2024-09-15T17:34:49+00:00 iffylaw/PIC: Permafrost Indices Computing Lihui Luo 2018-04-19 https://doi.org/10.5281/zenodo.1220663 unknown Zenodo https://github.com/iffylaw/PIC/tree/1.1 https://doi.org/10.5281/zenodo.1220662 https://doi.org/10.5281/zenodo.1220663 oai:zenodo.org:1220663 info:eu-repo/semantics/openAccess Other (Open) info:eu-repo/semantics/other 2018 ftzenodo https://doi.org/10.5281/zenodo.122066310.5281/zenodo.1220662 2024-07-25T12:53:33Z An R package permafrost indices computing (PIC) was developed, which integrates meteorological observations, remote sensing data, and field measurements to compute the factors or indices of permafrost and seasonal frozen soil. At present, 16 temperature/depth-related indices are integrated into the R package PIC to estimate the possible change trends of frozen soil in the Qinghai–Tibet Plateau (QTP). These indices include the mean annual air temperature, mean annual ground surface temperature, mean annual ground temperature, seasonal thawing/freezing n factor (nt/nf), thawing/freezing degree-days of air and ground surface (DDTa/DDTs/DDFa/DDFs), temperature at the top of the permafrost, active layer thickness, and maximum seasonal freeze depth. Other/Unknown Material Active layer thickness permafrost Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description An R package permafrost indices computing (PIC) was developed, which integrates meteorological observations, remote sensing data, and field measurements to compute the factors or indices of permafrost and seasonal frozen soil. At present, 16 temperature/depth-related indices are integrated into the R package PIC to estimate the possible change trends of frozen soil in the Qinghai–Tibet Plateau (QTP). These indices include the mean annual air temperature, mean annual ground surface temperature, mean annual ground temperature, seasonal thawing/freezing n factor (nt/nf), thawing/freezing degree-days of air and ground surface (DDTa/DDTs/DDFa/DDFs), temperature at the top of the permafrost, active layer thickness, and maximum seasonal freeze depth.
format Other/Unknown Material
author Lihui Luo
spellingShingle Lihui Luo
iffylaw/PIC: Permafrost Indices Computing
author_facet Lihui Luo
author_sort Lihui Luo
title iffylaw/PIC: Permafrost Indices Computing
title_short iffylaw/PIC: Permafrost Indices Computing
title_full iffylaw/PIC: Permafrost Indices Computing
title_fullStr iffylaw/PIC: Permafrost Indices Computing
title_full_unstemmed iffylaw/PIC: Permafrost Indices Computing
title_sort iffylaw/pic: permafrost indices computing
publisher Zenodo
publishDate 2018
url https://doi.org/10.5281/zenodo.1220663
genre Active layer thickness
permafrost
genre_facet Active layer thickness
permafrost
op_relation https://github.com/iffylaw/PIC/tree/1.1
https://doi.org/10.5281/zenodo.1220662
https://doi.org/10.5281/zenodo.1220663
oai:zenodo.org:1220663
op_rights info:eu-repo/semantics/openAccess
Other (Open)
op_doi https://doi.org/10.5281/zenodo.122066310.5281/zenodo.1220662
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