Conditions for thermal circulation in urban street canyons
Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Dallman, Ann [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Schlagwörter: |
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| Umfang: |
8 |
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| Übergeordnetes Werk: |
Enthalten in: Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A - Li, Huilin ELSEVIER, 2018, the international journal of building science and its applications, New York, NY [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:80 ; year:2014 ; pages:184-191 ; extent:8 |
| Links: |
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| DOI / URN: |
10.1016/j.buildenv.2014.05.014 |
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ELV022721037 |
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| 520 | |a Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. | ||
| 520 | |a Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. | ||
| 650 | 7 | |a Street canyon |2 Elsevier | |
| 650 | 7 | |a Atmospheric flows |2 Elsevier | |
| 650 | 7 | |a Urban canyon |2 Elsevier | |
| 650 | 7 | |a Buoyancy |2 Elsevier | |
| 650 | 7 | |a Thermal effects |2 Elsevier | |
| 650 | 7 | |a Dynamical regimes |2 Elsevier | |
| 700 | 1 | |a Magnusson, S. |4 oth | |
| 700 | 1 | |a Britter, R. |4 oth | |
| 700 | 1 | |a Norford, L. |4 oth | |
| 700 | 1 | |a Entekhabi, D. |4 oth | |
| 700 | 1 | |a Fernando, H.J.S. |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier |a Li, Huilin ELSEVIER |t Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A |d 2018 |d the international journal of building science and its applications |g New York, NY [u.a.] |w (DE-627)ELV000477206 |
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10.1016/j.buildenv.2014.05.014 doi GBVA2014011000024.pica (DE-627)ELV022721037 (ELSEVIER)S0360-1323(14)00150-4 DE-627 ger DE-627 rakwb eng 690 690 DE-600 570 VZ Dallman, Ann verfasserin aut Conditions for thermal circulation in urban street canyons 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Street canyon Elsevier Atmospheric flows Elsevier Urban canyon Elsevier Buoyancy Elsevier Thermal effects Elsevier Dynamical regimes Elsevier Magnusson, S. oth Britter, R. oth Norford, L. oth Entekhabi, D. oth Fernando, H.J.S. oth Enthalten in Elsevier Li, Huilin ELSEVIER Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A 2018 the international journal of building science and its applications New York, NY [u.a.] (DE-627)ELV000477206 volume:80 year:2014 pages:184-191 extent:8 https://doi.org/10.1016/j.buildenv.2014.05.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 80 2014 184-191 8 045F 690 |
| spelling |
10.1016/j.buildenv.2014.05.014 doi GBVA2014011000024.pica (DE-627)ELV022721037 (ELSEVIER)S0360-1323(14)00150-4 DE-627 ger DE-627 rakwb eng 690 690 DE-600 570 VZ Dallman, Ann verfasserin aut Conditions for thermal circulation in urban street canyons 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Street canyon Elsevier Atmospheric flows Elsevier Urban canyon Elsevier Buoyancy Elsevier Thermal effects Elsevier Dynamical regimes Elsevier Magnusson, S. oth Britter, R. oth Norford, L. oth Entekhabi, D. oth Fernando, H.J.S. oth Enthalten in Elsevier Li, Huilin ELSEVIER Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A 2018 the international journal of building science and its applications New York, NY [u.a.] (DE-627)ELV000477206 volume:80 year:2014 pages:184-191 extent:8 https://doi.org/10.1016/j.buildenv.2014.05.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 80 2014 184-191 8 045F 690 |
| allfields_unstemmed |
10.1016/j.buildenv.2014.05.014 doi GBVA2014011000024.pica (DE-627)ELV022721037 (ELSEVIER)S0360-1323(14)00150-4 DE-627 ger DE-627 rakwb eng 690 690 DE-600 570 VZ Dallman, Ann verfasserin aut Conditions for thermal circulation in urban street canyons 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Street canyon Elsevier Atmospheric flows Elsevier Urban canyon Elsevier Buoyancy Elsevier Thermal effects Elsevier Dynamical regimes Elsevier Magnusson, S. oth Britter, R. oth Norford, L. oth Entekhabi, D. oth Fernando, H.J.S. oth Enthalten in Elsevier Li, Huilin ELSEVIER Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A 2018 the international journal of building science and its applications New York, NY [u.a.] (DE-627)ELV000477206 volume:80 year:2014 pages:184-191 extent:8 https://doi.org/10.1016/j.buildenv.2014.05.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 80 2014 184-191 8 045F 690 |
| allfieldsGer |
10.1016/j.buildenv.2014.05.014 doi GBVA2014011000024.pica (DE-627)ELV022721037 (ELSEVIER)S0360-1323(14)00150-4 DE-627 ger DE-627 rakwb eng 690 690 DE-600 570 VZ Dallman, Ann verfasserin aut Conditions for thermal circulation in urban street canyons 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Street canyon Elsevier Atmospheric flows Elsevier Urban canyon Elsevier Buoyancy Elsevier Thermal effects Elsevier Dynamical regimes Elsevier Magnusson, S. oth Britter, R. oth Norford, L. oth Entekhabi, D. oth Fernando, H.J.S. oth Enthalten in Elsevier Li, Huilin ELSEVIER Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A 2018 the international journal of building science and its applications New York, NY [u.a.] (DE-627)ELV000477206 volume:80 year:2014 pages:184-191 extent:8 https://doi.org/10.1016/j.buildenv.2014.05.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 80 2014 184-191 8 045F 690 |
| allfieldsSound |
10.1016/j.buildenv.2014.05.014 doi GBVA2014011000024.pica (DE-627)ELV022721037 (ELSEVIER)S0360-1323(14)00150-4 DE-627 ger DE-627 rakwb eng 690 690 DE-600 570 VZ Dallman, Ann verfasserin aut Conditions for thermal circulation in urban street canyons 2014transfer abstract 8 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. Street canyon Elsevier Atmospheric flows Elsevier Urban canyon Elsevier Buoyancy Elsevier Thermal effects Elsevier Dynamical regimes Elsevier Magnusson, S. oth Britter, R. oth Norford, L. oth Entekhabi, D. oth Fernando, H.J.S. oth Enthalten in Elsevier Li, Huilin ELSEVIER Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A 2018 the international journal of building science and its applications New York, NY [u.a.] (DE-627)ELV000477206 volume:80 year:2014 pages:184-191 extent:8 https://doi.org/10.1016/j.buildenv.2014.05.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 80 2014 184-191 8 045F 690 |
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English |
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Enthalten in Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A New York, NY [u.a.] volume:80 year:2014 pages:184-191 extent:8 |
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Enthalten in Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A New York, NY [u.a.] volume:80 year:2014 pages:184-191 extent:8 |
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Integration-free reprogramming of human umbilical arterial endothelial cells into induced pluripotent stem cells IHSTMi001-A |
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Dallman, Ann @@aut@@ Magnusson, S. @@oth@@ Britter, R. @@oth@@ Norford, L. @@oth@@ Entekhabi, D. @@oth@@ Fernando, H.J.S. @@oth@@ |
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conditions for thermal circulation in urban street canyons |
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Conditions for thermal circulation in urban street canyons |
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Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. |
| abstractGer |
Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. |
| abstract_unstemmed |
Under conditions of low background winds and high solar radiation, non-uniform heating of building walls and the ground in an urban street canyon may induce thermally driven circulation that competes with inertially driven circulation due to overlying winds. These two types of circulation were studied using a field experiment, wherein a mock building canyon constructed with two rows of north–south aligned shipping containers were subjected to natural differential wall heating and overlying winds of varying magnitude. The site was carefully instrumented, and the measurements and flow visualization were conducted over nine days with varying environmental conditions. A buoyancy parameter, B = ( g α Δ T H ) / ( u 0 2 [ 1 + ( H / L ) 2 ] ) , where gαΔT is the horizontal anomaly of buoyancy arising from differential heating of canyon walls, H the canyon height, L the canyon width and u 0 the background velocity, was derived to demarcate thermal and inertial circulation regimes. When B < B c , where B c (≈0.05) is a critical value, the inertial circulation prevails, and the canyon velocities scaled by u 0 are approximately constant. When B > B c , the thermal circulation becomes important and at B ≫ B c , the flow is expected to be independent of u 0. An intermediate regime is found in the proximity of B c , where the scaled velocity is dependent both on overlying flow and buoyancy effects. |
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Conditions for thermal circulation in urban street canyons |
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