LIAN Jianbin,LI Shaoheng,CHEN Jianyao,et al.The identification of the influence of heat tracing method on underground temperature in the urbanization process of Guangzhou[J].Acta Scientiarum Naturalium Universitatis Sunyatseni,2024,63(04):29-36.
LIAN Jianbin,LI Shaoheng,CHEN Jianyao,et al.The identification of the influence of heat tracing method on underground temperature in the urbanization process of Guangzhou[J].Acta Scientiarum Naturalium Universitatis Sunyatseni,2024,63(04):29-36. DOI: 10.13471/j.cnki.acta.snus.ZR20230044.
The identification of the influence of heat tracing method on underground temperature in the urbanization process of Guangzhou
The intrinsic energy exchange exists between the shallow ground temperature and near-surface air temperature.As time progresses, surface temperature changes are propagated downwards and superimposed onto the steady-state geothermal field.Therefore, it is possible to reconstruct the history of ground surface temperature changes using the current subsurface temperature profile. To assess the combined effect of global warming and urbanization on the subsurface temperature of Guangzhou, this paper collected temperature data from Guangzhou station during 1958-2022 and conducted regression analysis and anomaly analysis. Meanwhile, the temperature-depth (T-Z) profiles of 16 observation boreholes in Guangzhou were obtained through field measurements. By conducting regression analysis on the lower section of the temperature profile, the geothermal gradient of the area and the depth of deviation from the constant geothermal gradient were determined. Finally,the onset time and magnitude of warming were obtained by combining temperature data, and the theoretical curves of the surface warming profile in Guangzhou were derived using the analytical solution equation. The results show that the warming rate of air temperature in Guangzhou from 1958 to 2022 is 0.33 ℃ per decade, with the onset time of warming being 1987, and the magnitude of warming being 2.6 ℃.The observed geothermal gradient in Guangzhou is 0.036 ℃/m, and the depth of deviation from the constant geothermal gradient is 54.8 m, essentially consistent with the analytically calculated depth of 57.6 m. The study finds that the earlier the start time of urbanization-induced surface warming, the greater the depth of deviation of subsurface temperature from the constant geothermal gradient, indicating the depth of deviation can be used to describe the process of urbanization.
关键词
全球变暖城市化气温地温广州
Keywords
global warmingurbanizationair temperatureground temperatureGuangzhou
ANDERSON M P,2005.Heat as a ground water tracer[J].Ground Water, 43(6):951-968.
BIRCH A F, 1948.The effects of Pleistocene climatic variations upon geothermal gradients[J].Am J Sci, 246(12):729-760.
FERGUSON G, WOODBURY A D,2004.Subsurface heat flow in an urban environment[J].J Geophys Res, 109(B2):B02402.
HARRIS R N, CHAPMAN D S, 1997.Borehole temperatures and a baseline for 20th-century global warming estimates[J].Science, 275(5306):1618-1621.
HUANG S, POLLACK H N, SHEN P Y, 2000.Temperature trends over the past five centuries reconstructed from borehole temperatures[J]. Nature, 403(6771):756-758.
KALNAY E,CAI M,2003.Impact of urbanization and land-use change on climate[J].Nature, 423:528-531.
LIU B, XU M, HENDERSON M, et al,2004.Taking China's temperature:Daily range, warming trends, and regional variations,1955-2000[J]. J Clim,17(22):4453-4462.
PARKER D E,2006.A demonstration that large-scale warming is not urban[J].J Clim, 19(12):2882-2895.
ROSENZWEIG C, KAROLY D,VICARELLI M, et al,2008.Attributing physical and biological impacts to anthropogenic climate change[J].Nature,453(7193):353-357.
SCHMIDT W L, GOSNOLD W D, ENZ J W, 2001.A decade of air-ground temperature exchange from Fargo,North Dakota[J].Glob Planet Change, 29(3/4):311-325.
SILLIMAN S E, BOOTH D F, 1993.Analysis of time-series measurements of sediment temperature for identification of Gaining vs.losing portions of Juday Creek, Indiana[J].J Hydrol, 146:131-148.
TANIGUCHI M, SHIMADA J, TANAKA T, et al, 1999. Disturbances of temperature-depth profiles due to surface climate change and subsurface water flow:1. An effect of linear increase in surface temperature caused by global warming and urbanization in the Tokyo Metropolitan Area, Japan[J].Water Resour Res, 35(5):1507-1517.
TANIGUCHI M, UEMURA T, JAGO-ON K, 2007.Combined effects of urbanization and global warming on subsurface temperature in four Asian cities[J].Vadose Zone J, 6(3):591-596.
TANIGUCHI M,UEMURA T, 2005.Effects of urbanization and groundwater flow on the subsurface temperature in Osaka,Japan[J].Phys Earth Planet Inter,152(4):305-313.
TAYLOR C A, STEFAN H G, 2009. Shallow groundwater temperature response to climate change and urbanization[J].J Hydrol, 375(3):601-612.