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DWCZ - CO - Gordon Gulch 1 & 2, SWE along Snow Pole Transects (GG1-GG2-SWE) -- Gordon Gulch -- (2023)

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DataONE2023-11-08 更新2024-06-08 收录
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SWE measured by calibrated scale including mass of tube (cm) For North aspects, downslope is between the lowest snow pole and second-lowest snow pole. Upslope is between the highest snow pole and second-highest snow pole. For South aspects, data were collected between the two snow poles and this entry is left blank. LOCATION : Gordon Gulch (GG1) & (GG2) LOCATION DESCRIPTION: Gordon Gulch (2590 m) lies within Arapahoe National Forest and is divided into 1 (lower) and 2 (upper) Gordon Gulch._ Gordon Gulch joins the North Boulder Creek about 16 km downstream from Green Lakes Valley (GLV)._ This site is underlain by biotite gneiss and is mostly forested. Different aspect slopes present contrasts in soils and vegetation: thinner, less-weathered rock with grasses and Ponderosa pine (P. ponderosa) on south-facing slopes, and thicker, more weathered rock with dense Lodgepole pine (P. cortorta) on north-facing slopes. It is characterized by the low-relief remnants of a dissected Tertiary erosion surface in which weathered rock profiles are up to 15 m thick._ Gordon Gulch is within the montane climatic zone._MAP is 780 mm, 70% as snow. For North aspects, downslope is between the lowest snow pole and second-lowest snow pole. Upslope is between the highest snow pole and second-highest snow pole. For South aspects, data were collected between the two snow poles and this entry is left blank. Number of replicate done at each date *aspect* plot combinationnamic eatter

雪水当量(Snow Water Equivalent,SWE)采用包含管质量的校准标尺进行测量(单位:cm)。 对于北向坡面,下坡段处于最低雪杆与第二低雪杆之间;上坡段处于最高雪杆与第二高雪杆之间。对于南向坡面,数据采集于两根雪杆之间,且本条目留空。 研究地点:戈登峡谷(Gordon Gulch,GG1)与(GG2) 地点描述:戈登峡谷(海拔2590米)坐落于阿拉帕霍国家森林(Arapahoe National Forest)境内,被划分为下戈登峡谷(1号区域)与上戈登峡谷(2号区域)。戈登峡谷在绿湖谷(Green Lakes Valley,GLV)下游约16公里处汇入北博尔德溪。该区域基底为黑云母片麻岩,地表以森林覆盖为主。不同坡向的坡面在土壤与植被特征上存在显著差异:南向坡分布有更薄、风化程度更低的岩层,伴生草本植物与黄松(P. ponderosa);北向坡则分布有更厚、风化程度更高的岩层,伴生茂密的黑松(P. cortorta)。 该区域以经切割改造的第三纪侵蚀面低起伏残余地貌为典型特征,其风化岩层剖面厚度可达15米。 戈登峡谷属于山地气候带,年均降水量为780毫米,其中70%以降雪形式产出。 对于北向坡面,下坡段处于最低雪杆与第二低雪杆之间;上坡段处于最高雪杆与第二高雪杆之间。对于南向坡面,数据采集于两根雪杆之间,且本条目留空。 各日期*坡向*样地组合的重复采样次数
创建时间:
2023-12-30
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