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Study on the Change in Freezing Depth in Heilongjiang Province and Its Response to Winter Half-Year Temperature

dc.contributor.authorFanxiang Meng
dc.contributor.authorZongliang Wang
dc.contributor.authorQiang Fu
dc.contributor.authorTianxiao Li
dc.contributor.authorXu Yang
dc.contributor.authorEnnan Zheng
dc.contributor.authorGe Zhang
dc.contributor.authorQing Zhuang
dc.contributor.authorQiyang Fu
dc.contributor.authorYuan Zhang
dc.date.accessioned2023-04-12T18:28:02Z
dc.date.available2023-04-12T18:28:02Z
dc.date.copyright2022/08/01
dc.date.issued2022
dc.identifier.otherJAMC-D-21-0195.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289716
dc.description.abstractThe evolution of the average freezing depth and maximum freezing depth of seasonal frozen soil and their correlations with the average winter half-year temperature in Heilongjiang Province in China are analyzed. Linear regression, the Mann–Kendall test, and kriging interpolation are applied to freezing depth data from 20 observation stations in Heilongjiang Province from 1972 to 2016 and daily average temperature data from 34 national meteorological stations collected in the winters of 1972–2020. The results show that the average freezing depth decreases at a rate of 4.8 cm (10 yr)
dc.publisherAmerican Meteorological Society
dc.titleStudy on the Change in Freezing Depth in Heilongjiang Province and Its Response to Winter Half-Year Temperature
dc.typeJournal Paper
dc.journal.volume61
dc.journal.issue8
dc.journal.titleJournal of Applied Meteorology and Climatology
dc.identifier.doi10.1175/JAMC-D-21-0195.1
dc.journal.fristpage1003
dc.journal.lastpage1013
dc.page1003–1013
dc.treeJournal of Applied Meteorology and Climatology:;2022:;volume( 061 ):;issue: 008
dc.contenttypeFulltext


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