Reply to discussion on ‘Borehole temperature log from the Glasgow Geothermal Energy Research Field Site: a record of past changes to ground surface temperature caused by urban development’ by Watson and Westaway 2020 (SJG, 56, 134–152)

IF 0.5 4区 地球科学 Q4 GEOLOGY
R. Westaway
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引用次数: 0

Abstract

Watson and Westaway (2020) (WW) quantified subsurface temperature variations caused by anthropogenic climate change and urban/industrial development in Glasgow, using temperature data from the Glasgow Geothermal Energy Research Field Site (GGERFS) well GGC-01 (at site G-10; Fig. 1), noting implications for the thermal physics of this site. Monaghan et al. (2021) (MMS) have queried points, noted in passing by WW, on other aspects: the GGERFS purpose, location, design, heat resource and cost.
对Watson和Westaway 2020(SJG,56134-152)关于“格拉斯哥地热能研究现场钻孔温度日志:城市发展导致地表温度过去变化的记录”的讨论的回复
Watson和Westaway(2020)(WW)利用格拉斯哥地热能研究现场(GGERFS)GGC-01井(位于G-10;图1)的温度数据,量化了人为气候变化和格拉斯哥城市/工业发展引起的地下温度变化,并指出了对该现场热物理的影响。Monaghan等人(2021)(MMS)对WW顺便指出的其他方面提出了质疑:GGERFS的目的、位置、设计、热资源和成本。
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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