Comparison of cooling effect between green space and water body

The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selec...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Tan, Xingyu [verfasserIn] Sun, Xiang [verfasserIn] Huang, Chengdao [verfasserIn] Yuan, Yuan [verfasserIn] Hou, Donglin [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	Urban heat island Green space Water body Cooling range Cooling intensity

Übergeordnetes Werk:	Enthalten in: Sustainable cities and society - Amsterdam [u.a.] : Elsevier, 2011, 67
Übergeordnetes Werk:	volume:67

DOI / URN:	10.1016/j.scs.2021.102711

Katalog-ID:	ELV005759684

Internformat


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520			\|a The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces.
650		4	\|a Urban heat island
650		4	\|a Green space
650		4	\|a Water body
650		4	\|a Cooling range
650		4	\|a Cooling intensity
700	1		\|a Sun, Xiang \|e verfasserin \|4 aut
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700	1		\|a Hou, Donglin \|e verfasserin \|4 aut
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912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_224
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2006
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912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
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912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2088
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2470
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4046
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4322
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4325
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
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952			\|d 67

Indexfelder

author_variant	x t xt x s xs c h ch y y yy d h dh
matchkey_str	tanxingyusunxianghuangchengdaoyuanyuanho:2021----:oprsnfolnefcbtenres
hierarchy_sort_str	2021
publishDate	2021
allfields	10.1016/j.scs.2021.102711 doi (DE-627)ELV005759684 (ELSEVIER)S2210-6707(21)00006-8 DE-627 ger DE-627 rda eng 690 720 DE-600 Tan, Xingyu verfasserin aut Comparison of cooling effect between green space and water body 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces. Urban heat island Green space Water body Cooling range Cooling intensity Sun, Xiang verfasserin aut Huang, Chengdao verfasserin aut Yuan, Yuan verfasserin aut Hou, Donglin verfasserin aut Enthalten in Sustainable cities and society Amsterdam [u.a.] : Elsevier, 2011 67 Online-Ressource (DE-627)635602792 (DE-600)2573417-9 (DE-576)336956703 nnns volume:67 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 AR 67
spelling	10.1016/j.scs.2021.102711 doi (DE-627)ELV005759684 (ELSEVIER)S2210-6707(21)00006-8 DE-627 ger DE-627 rda eng 690 720 DE-600 Tan, Xingyu verfasserin aut Comparison of cooling effect between green space and water body 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces. Urban heat island Green space Water body Cooling range Cooling intensity Sun, Xiang verfasserin aut Huang, Chengdao verfasserin aut Yuan, Yuan verfasserin aut Hou, Donglin verfasserin aut Enthalten in Sustainable cities and society Amsterdam [u.a.] : Elsevier, 2011 67 Online-Ressource (DE-627)635602792 (DE-600)2573417-9 (DE-576)336956703 nnns volume:67 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 AR 67
allfields_unstemmed	10.1016/j.scs.2021.102711 doi (DE-627)ELV005759684 (ELSEVIER)S2210-6707(21)00006-8 DE-627 ger DE-627 rda eng 690 720 DE-600 Tan, Xingyu verfasserin aut Comparison of cooling effect between green space and water body 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces. Urban heat island Green space Water body Cooling range Cooling intensity Sun, Xiang verfasserin aut Huang, Chengdao verfasserin aut Yuan, Yuan verfasserin aut Hou, Donglin verfasserin aut Enthalten in Sustainable cities and society Amsterdam [u.a.] : Elsevier, 2011 67 Online-Ressource (DE-627)635602792 (DE-600)2573417-9 (DE-576)336956703 nnns volume:67 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 AR 67
allfieldsGer	10.1016/j.scs.2021.102711 doi (DE-627)ELV005759684 (ELSEVIER)S2210-6707(21)00006-8 DE-627 ger DE-627 rda eng 690 720 DE-600 Tan, Xingyu verfasserin aut Comparison of cooling effect between green space and water body 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces. Urban heat island Green space Water body Cooling range Cooling intensity Sun, Xiang verfasserin aut Huang, Chengdao verfasserin aut Yuan, Yuan verfasserin aut Hou, Donglin verfasserin aut Enthalten in Sustainable cities and society Amsterdam [u.a.] : Elsevier, 2011 67 Online-Ressource (DE-627)635602792 (DE-600)2573417-9 (DE-576)336956703 nnns volume:67 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 AR 67
allfieldsSound	10.1016/j.scs.2021.102711 doi (DE-627)ELV005759684 (ELSEVIER)S2210-6707(21)00006-8 DE-627 ger DE-627 rda eng 690 720 DE-600 Tan, Xingyu verfasserin aut Comparison of cooling effect between green space and water body 2021 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces. Urban heat island Green space Water body Cooling range Cooling intensity Sun, Xiang verfasserin aut Huang, Chengdao verfasserin aut Yuan, Yuan verfasserin aut Hou, Donglin verfasserin aut Enthalten in Sustainable cities and society Amsterdam [u.a.] : Elsevier, 2011 67 Online-Ressource (DE-627)635602792 (DE-600)2573417-9 (DE-576)336956703 nnns volume:67 GBV_USEFLAG_U SYSFLAG_U GBV_ELV GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 AR 67
language	English
source	Enthalten in Sustainable cities and society 67 volume:67
sourceStr	Enthalten in Sustainable cities and society 67 volume:67
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Urban heat island Green space Water body Cooling range Cooling intensity
dewey-raw	690
isfreeaccess_bool	false
container_title	Sustainable cities and society
authorswithroles_txt_mv	Tan, Xingyu @@aut@@ Sun, Xiang @@aut@@ Huang, Chengdao @@aut@@ Yuan, Yuan @@aut@@ Hou, Donglin @@aut@@
publishDateDaySort_date	2021-01-01T00:00:00Z
hierarchy_top_id	635602792
dewey-sort	3690
id	ELV005759684
language_de	englisch
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author	Tan, Xingyu
spellingShingle	Tan, Xingyu ddc 690 misc Urban heat island misc Green space misc Water body misc Cooling range misc Cooling intensity Comparison of cooling effect between green space and water body
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topic_title	690 720 DE-600 Comparison of cooling effect between green space and water body Urban heat island Green space Water body Cooling range Cooling intensity
topic	ddc 690 misc Urban heat island misc Green space misc Water body misc Cooling range misc Cooling intensity
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title	Comparison of cooling effect between green space and water body
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title_full	Comparison of cooling effect between green space and water body
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title_sort	comparison of cooling effect between green space and water body
title_auth	Comparison of cooling effect between green space and water body
abstract	The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces.
abstractGer	The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces.
abstract_unstemmed	The cooling effects of green spaces and water bodies are essential in subtropical cities with high temperatures combined with increasing urban heat island effect, while there is insufficient research on the difference between these two categories of cold sources. Therefore, Nanning, China, was selected as the typical case in the subtropical climate zone, and spatial and statistical analysis based on Landsat 8 OLI/TIRS images was conducted to compare the cooling effect and factors of blue and green spaces. Results showed that (1) the area-related green-space and water-body metrics are significantly positively correlated with the cooling effect. An additional 10 % of green space cover leads to a decline in the mean LST of 0.39 °C compared with a decline of 0.42 °C for water cover; (2) green and blue spaces with simple shapes and high fragmentation may have strong cooling effect, whereas green and blue spaces with more complex shapes may cool larger areas, benefiting more residents; (3) the threshold values of efficiency (TVoE) of tree-based green spaces and water patches were both approximately 0.30 ha, increasing with spatial sprawl of impervious surfaces; and (4) water bodies have slightly higher cooling intensity and much larger cooling ranges than tree-based green spaces.
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title_short	Comparison of cooling effect between green space and water body
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author2	Sun, Xiang Huang, Chengdao Yuan, Yuan Hou, Donglin
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doi_str	10.1016/j.scs.2021.102711
up_date	2024-07-06T19:03:59.766Z
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Comparison of cooling effect between green space and water body

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