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Climate manipulation (warming and wetting) experiment in Cambridge Bay, Canada

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dc.contributor.authorJung, Ji Young-
dc.contributor.authorKwon, Min Jung-
dc.contributor.authorKim, Mincheol-
dc.contributor.authorKang, Hojeong-
dc.contributor.authorSeo, Juyoung-
dc.contributor.authorYun, Jeongeun-
dc.contributor.authorNam, Sungjin-
dc.contributor.authorLee, Yoo Kyung-
dc.date.accessioned2021-07-26T05:46:54Z-
dc.date.available2021-07-26T05:46:54Z-
dc.date.issued2018-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/12331-
dc.description.abstractAtmospheric temperature in the Arctic has increased more than the mid or low latitude, and this trend is expected to continue in the future. Precipitation pattern is also changing due to warming but more unpredictable. A number of studies have been carried out to investigate the responses of terrestrial ecosystems to increased temperature, but less have focused on the effects of precipitation changes or combined effects of temperature and precipitation. We conduct an experiment to examine the effects of both warming and increased summer precipitation on ecosystem characteristics in the Canadian high Arctic since 2012. The study site is located in Cambridge Bay on the southeast coast of Victoria Island, Nunavut (69° 07' 48" N, 105° 03' 35" W). The ecosystem is dry tundra composed of Carex spp. and Dryas integrifolia as dominant vegetation types. A climate manipulation experiment was designed in a factorial combination with warming (ambient vs. increased temperature) and precipitation (ambient vs. increased precipitation). The hexagon types of open top chambers (OTCs) in a 2-m diameter were used to increase temperature, and 2 L of water/per plot (4 m2 area) was added every week throughout summer. The OTCs increased ca. 1 and 0.5 °C of atmospheric and soil temperature, respectively. In 2018, we measure net ecosystem exchange and ecosystem respiration using a manual chamber method and extract dissolved organic carbon and inorganic nitrogen from June to September to observe both treatment effects and seasonal changes. We also analyze microbial biomass through extracting microbial phospholipid fatty acids and microbial activities by measuring extracellular enzyme activities. Plant cover is estimated using point-intercept method, and normalized difference vegetation index is measured throughout the summer. We expect to understand the single and combined effects of increased temperature and precipitation on soil biogeochemical processes with a link of changes in plant and microbial activities through synthesizing all the results produced in the previous and coming years.en_US
dc.languageEnglishen_US
dc.language.isoenen_US
dc.titleClimate manipulation (warming and wetting) experiment in Cambridge Bay, Canadaen_US
dc.title.alternative캐나다 캠브리지 베이의 기후변화 모사 실험en_US
dc.typePosteren_US
dc.identifier.bibliographicCitationJung, Ji Young, et al. 2018. Climate manipulation (warming and wetting) experiment in Cambridge Bay, Canada. AGU fall meeting 2018. Washington, D.C.. 2018.12.10~2018.12.14.-
dc.citation.conferenceDate2018.12.10~2018.12.14en_US
dc.citation.conferenceNameAGU fall meeting 2018en_US
dc.citation.conferencePlaceWashington, D.C.en_US
dc.description.articleClassification포스터-
dc.identifier.localId2018-0435-
Appears in Collections  
2016-2018, Arctic permafrost environment change monitoring and prediction method developments (16-18) / Lee, Bang Yong (PN16081; PN17081; PN18081)
2018-2018, Arctic permafrost environment change monitoring and prediction method developments (18-18) / Lee, Bang Yong (PN18081)
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