The discontinuous permafrost region of northwestern Canada is experiencing rapid warming resulting in dramatic land cover change from forested peatland permafrost terrain to treeless wetlands. Extensive research has been conducted throughout this region to gain insight into how climate‐induced land cover change will impact water resources and ecosystem function. This paper presents a hydrological and micrometeorological dataset collected in the Scotty Creek basin, Northwest Territories, Canada over the period of 01 October 2014 to 30 September 2015, a sample of the intensive and coordinated measurements collected annually at this site. Micrometeorological data collected from four stations, one located in each of the land cover types representative of those comprising the Scotty Creek basin including bog, channel fen, stable peat plateau and peat plateau undergoing rapid permafrost degradation and loss, are presented. Monitored micrometeorological variables include incoming and outgoing shortwave and longwave radiation, air temperature, relative humidity, wind speed, precipitation (rain and snow) and snow depth. Deep ground temperatures (~1–10 m below the ground surface) from a channel fen as well as disturbed sites common to the basin including a seismic line and winter road are presented. Water levels were also monitored in the representative land cover types over this period. This dataset is available from the Wilfrid Laurier University Library Research Data Repository (https://doi.org/10.5683/SP/OQDRJG) and can be used in coordination with other hydrological and micrometeorological datasets to examine spatio‐temporal effects of meteorological conditions on local hydrological responses across cold regions.

中文翻译：

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加拿大西北地区斯科蒂溪的泥炭地为主的不连续多年冻土的水文气象测量

加拿大西北部不连续的多年冻土地区正在经历快速变暖，导致土地覆盖范围发生了戏剧性的变化，从森林泥炭地多年冻土地形变为无树湿地。在整个地区进行了广泛的研究，以了解气候引起的土地覆盖变化将如何影响水资源和生态系统功能。本文介绍了2014年10月1日至2015年9月30日期间在加拿大西北地区斯科蒂克里克盆地收集的水文和微气象数据集，该地点每年进行密集和协调的测量。从四个站点收集的微气象数据，每个站点位于代表包括Scotty Creek盆地（包括沼泽，芬河，介绍了稳定的泥炭高原和经历快速多年冻土退化和损失的泥炭高原。监测的微气象变量包括传入和传出的短波和长波辐射，气温，相对湿度，风速，降水（雨雪）和雪深。给出了河道的深部地面温度（地下约1-10 m）以及盆地常见的受干扰地点，包括地震测线和冬季道路。在此期间，还监测了代表性土地覆盖类型的水位。该数据集可从Wilfrid Laurier大学图书馆研究数据存储库（https://doi.org/10。