seasonal thawing index
Link: http://w3id.org/permafrost/v/ipaglossary/t0287
Within: IPA Permafrost Glossary
Definition: The cumulative number of degree-days above 0°C, calculated as the arithmetic sum of all the positive and negative mean daily air temperatures (°C) for a specific station during the time period between the lowest point in the spring and the highest point the next fall on the cumulative degree-day time curve.
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seasonal thawing index
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https://doi.org/10.4224/20386561
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