Hydrometeorological data from Marmot Creek Research Basin, Canadian Rockies
Hydrometeorological data from Marmot Creek Research Basin, Canadian Rockies
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来自加拿大落基山脉 Marmot Creek 研究盆地的水文气象数据
DOI：
10.5194/essd-11-455-2019
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发表时间：
2018
影响因子：
11.4
通讯作者：
Evan Siemens
中科院分区：
文献类型：
--
作者：
X. Fang;J. Pomeroy;C. DeBeer;P. Harder;Evan Siemens
抽象的。提供气象、雪调查、径流和地下水数据
来自加拿大艾伯塔省土拨鼠溪研究盆地。盆地是一个
9.4平方公里，萨斯喀彻温省高山-山地森林源头流域
为草原省份提供重要供水的河流流域
加拿大。它经过大量仪器仪表化、实验和操作
1962 年至 1986 年间，多个联邦政府机构
其主要流域和次流域均设有测量自动化气象站
在多个标高安装了地下水观测井
以及自动和频繁的手动测量积雪和
进行了消融以及其他天气和水变量。在此期间，
两个子盆地成熟的常绿森林被砍伐，留下大片
一个盆地的砍伐和一个“蜂窝”的小型森林空地
另一个盆地。同时气象测量和子流域径流
流域内的排放堰在 20 世纪 80 年代末被拆除，联邦
政府维持出口水流流量测量和
附近的高海拔气象站和阿尔伯塔省
政府维护了观测井和附近的一个火灾气象站。
Marmot Creek 研究盆地大规模重新安装了 12 个自动化仪器
气象站、四个子流域水文测站和七个雪地
萨斯喀彻温大学中心于 2004 年开始进行的调查横断面
用于水文学。观测提供了有关气象的详细信息，
降水量、土壤湿度、积雪、径流和地下水
1962年至1987年的历史时期和2005年至2005年的现代时期
现在的时间。这些数据非常适合监测气候变化，
加深对水文过程的理解，评估过程算法
和水文、冰冻圈或大气模型，并检查
流域水文循环对气候、极端气候变化的响应
通过水文建模和统计来确定天气和土地覆盖
分析。所提供的数据可从联邦研究中心公开获取
数据存储库（https://doi.org/10.20383/101.09，Fang 等人，2018）。
Abstract. Meteorological, snow survey, streamflow, and groundwater data are presented
from Marmot Creek Research Basin, Alberta, Canada. The basin is a
9.4 km2, alpine–montane forest headwater catchment of the Saskatchewan
River basin that provides vital water supplies to the Prairie Provinces of
Canada. It was heavily instrumented, experimented upon, and operated by
several federal government agencies between 1962 and 1986, during which time
its main and sub-basin streams were gauged, automated meteorological stations
at multiple elevations were installed, groundwater observation wells were dug
and automated, and frequent manual measurements of snow accumulation and
ablation and other weather and water variables were made. Over this period,
mature evergreen forests were harvested in two sub-basins, leaving large
clear cuts in one basin and a “honeycomb” of small forest clearings in
another basin. Whilst meteorological measurements and sub-basin streamflow
discharge weirs in the basin were removed in the late 1980s, the federal
government maintained the outlet streamflow discharge measurements and a
nearby high-elevation meteorological station, and the Alberta provincial
government maintained observation wells and a nearby fire weather station.
Marmot Creek Research Basin was intensively re-instrumented with 12 automated
meteorological stations, four sub-basin hydrometric sites, and seven snow
survey transects starting in 2004 by the University of Saskatchewan Centre
for Hydrology. The observations provide detailed information on meteorology,
precipitation, soil moisture, snowpack, streamflow, and groundwater during
the historical period from 1962 to 1987 and the modern period from 2005 to
the present time. These data are ideal for monitoring climate change,
developing hydrological process understanding, evaluating process algorithms
and hydrological, cryospheric, or atmospheric models, and examining the
response of basin hydrological cycling to changes in climate, extreme
weather, and land cover through hydrological modelling and statistical
analyses. The data presented are publicly available from Federated Research
Data Repository (https://doi.org/10.20383/101.09, Fang et al., 2018).
加拿大落基山脉针叶林覆盖对辐射和融雪动态的影响
影响因子：
2.2
作者：
Ellis C
通讯作者：
Ellis C