FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1499833836> ?p ?o ?g. }

• W1499833836 endingPage "118" @default.
• W1499833836 startingPage "103" @default.
• W1499833836 abstract "Permafrost conditions were examined between 2010 and 2014 at four sites across an alpine treeline on Peel Plateau, Northwest Territories, Canada. Ground and air temperature sensors were installed in forest and tundra between 30 and 500 m asl. Annual mean air temperatures increased and the number of freezing degree days declined with elevation, due to persistent winter air temperature inversions. The annual mean temperature at the permafrost surface (Tps) in mineral soils increased with elevation from about −2.5 °C in lowland forest to about −1.5 °C in dwarf shrub tundra. The increase in Tps coincided with higher air temperatures and earlier snow accumulation at tundra sites. The higher Tps in alpine tundra compared to lowland forest in Peel Plain contrasts with the northward decrease in Tps across latitudinal treeline elsewhere in the western Arctic. An increase in Tps with elevation may be common in Arctic mountain environments due to the prevalence of atmospheric temperature inversions in winter. In such contexts, although vegetation characteristics are governed by summer climate, permafrost conditions are critically influenced by the winter regime. The tundra permafrost on Peel Plateau is considerably warmer and, hence, more sensitive to disturbance than perennially frozen ground north of treeline in other parts of the western Arctic. Copyright © 2015 John Wiley & Sons, Ltd." @default.
• W1499833836 created "2016-06-24" @default.
• W1499833836 creator A5004676605 @default.
• W1499833836 creator A5045168402 @default.
• W1499833836 creator A5048299964 @default.
• W1499833836 creator A5077114740 @default.
• W1499833836 date "2015-03-17" @default.
• W1499833836 modified "2023-09-29" @default.
• W1499833836 title "‘Warm’ Tundra: Atmospheric and Near-Surface Ground Temperature Inversions Across an Alpine Treeline in Continuous Permafrost, Western Arctic, Canada" @default.
• W1499833836 cites W1488616880 @default.
• W1499833836 cites W1550726078 @default.
• W1499833836 cites W1567365373 @default.
• W1499833836 cites W1584831867 @default.
• W1499833836 cites W178907388 @default.
• W1499833836 cites W1867191789 @default.
• W1499833836 cites W1950558152 @default.
• W1499833836 cites W1963683409 @default.
• W1499833836 cites W1968880765 @default.
• W1499833836 cites W1981776080 @default.
• W1499833836 cites W1987603884 @default.
• W1499833836 cites W2026784405 @default.
• W1499833836 cites W2029152579 @default.
• W1499833836 cites W2049615096 @default.
• W1499833836 cites W2051188999 @default.
• W1499833836 cites W2052856745 @default.
• W1499833836 cites W2070979892 @default.
• W1499833836 cites W2073631719 @default.
• W1499833836 cites W2081115654 @default.
• W1499833836 cites W2081586421 @default.
• W1499833836 cites W2091968803 @default.
• W1499833836 cites W2115893789 @default.
• W1499833836 cites W2146712817 @default.
• W1499833836 cites W2157026492 @default.
• W1499833836 cites W2168434255 @default.
• W1499833836 cites W2173582002 @default.
• W1499833836 cites W2312247695 @default.
• W1499833836 cites W2325211438 @default.
• W1499833836 cites W2335465793 @default.
• W1499833836 cites W2981451752 @default.
• W1499833836 cites W3140270738 @default.
• W1499833836 cites W4239456067 @default.
• W1499833836 cites W44197508 @default.
• W1499833836 cites W623950296 @default.
• W1499833836 cites W74135275 @default.
• W1499833836 doi "https://doi.org/10.1002/ppp.1838" @default.
• W1499833836 hasPublicationYear "2015" @default.
• W1499833836 type Work @default.
• W1499833836 sameAs 1499833836 @default.
• W1499833836 citedByCount "27" @default.
• W1499833836 countsByYear W14998338362015 @default.
• W1499833836 countsByYear W14998338362016 @default.
• W1499833836 countsByYear W14998338362017 @default.
• W1499833836 countsByYear W14998338362018 @default.
• W1499833836 countsByYear W14998338362019 @default.
• W1499833836 countsByYear W14998338362020 @default.
• W1499833836 countsByYear W14998338362021 @default.
• W1499833836 countsByYear W14998338362023 @default.
• W1499833836 crossrefType "journal-article" @default.
• W1499833836 hasAuthorship W1499833836A5004676605 @default.
• W1499833836 hasAuthorship W1499833836A5045168402 @default.
• W1499833836 hasAuthorship W1499833836A5048299964 @default.
• W1499833836 hasAuthorship W1499833836A5077114740 @default.
• W1499833836 hasConcept C100970517 @default.
• W1499833836 hasConcept C111368507 @default.
• W1499833836 hasConcept C114793014 @default.
• W1499833836 hasConcept C125069764 @default.
• W1499833836 hasConcept C127313418 @default.
• W1499833836 hasConcept C132651083 @default.
• W1499833836 hasConcept C134306372 @default.
• W1499833836 hasConcept C142724271 @default.
• W1499833836 hasConcept C15098985 @default.
• W1499833836 hasConcept C18903297 @default.
• W1499833836 hasConcept C197046000 @default.
• W1499833836 hasConcept C205649164 @default.
• W1499833836 hasConcept C2524010 @default.
• W1499833836 hasConcept C2776133958 @default.
• W1499833836 hasConcept C2778091200 @default.
• W1499833836 hasConcept C2780030769 @default.
• W1499833836 hasConcept C2780155556 @default.
• W1499833836 hasConcept C2983363897 @default.
• W1499833836 hasConcept C30878456 @default.
• W1499833836 hasConcept C33923547 @default.
• W1499833836 hasConcept C37054046 @default.
• W1499833836 hasConcept C39432304 @default.
• W1499833836 hasConcept C49204034 @default.
• W1499833836 hasConcept C518008717 @default.
• W1499833836 hasConcept C71924100 @default.
• W1499833836 hasConcept C86803240 @default.
• W1499833836 hasConceptScore W1499833836C100970517 @default.
• W1499833836 hasConceptScore W1499833836C111368507 @default.
• W1499833836 hasConceptScore W1499833836C114793014 @default.
• W1499833836 hasConceptScore W1499833836C125069764 @default.
• W1499833836 hasConceptScore W1499833836C127313418 @default.
• W1499833836 hasConceptScore W1499833836C132651083 @default.
• W1499833836 hasConceptScore W1499833836C134306372 @default.
• W1499833836 hasConceptScore W1499833836C142724271 @default.
• W1499833836 hasConceptScore W1499833836C15098985 @default.
• W1499833836 hasConceptScore W1499833836C18903297 @default.

• next