2008
DOI: 10.1007/s00484-008-0162-7
|View full text |Cite
|
Sign up to set email alerts
|

SOLWEIG 1.0 – Modelling spatial variations of 3D radiant fluxes and mean radiant temperature in complex urban settings

Abstract: The mean radiant temperature, T(mrt), which sums up all shortwave and longwave radiation fluxes (both direct and reflected) to which the human body is exposed is one of the key meteorological parameters governing human energy balance and the thermal comfort of man. In this paper, a new radiation model (SOLWEIG 1.0), which simulates spatial variations of 3D radiation fluxes and T(mrt) in complex urban settings, is presented. The T(mrt) is derived by modelling shortwave and longwave radiation fluxes in six direc… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

3
197
0
5

Year Published

2010
2010
2020
2020

Publication Types

Select...
9

Relationship

2
7

Authors

Journals

citations
Cited by 381 publications
(205 citation statements)
references
References 23 publications
3
197
0
5
Order By: Relevance
“…the SOLWEIG model (Lindberg et al, 2008), RayMan (Matzarakis et al, 2010), the TUF-3D model (Krayenhoff and Voogt, 2007), the TUF-IOBES model (Yaghoobian and Kleissl, 2012, based on TUF-3D), TEB (Masson, 2000), or SUEWS (Järvi et al, 2011). These models treat some physical processes (e.g.…”
Section: Urban Climatementioning
confidence: 99%
“…the SOLWEIG model (Lindberg et al, 2008), RayMan (Matzarakis et al, 2010), the TUF-3D model (Krayenhoff and Voogt, 2007), the TUF-IOBES model (Yaghoobian and Kleissl, 2012, based on TUF-3D), TEB (Masson, 2000), or SUEWS (Järvi et al, 2011). These models treat some physical processes (e.g.…”
Section: Urban Climatementioning
confidence: 99%
“…Several methods are available to calculate the SVF based on fisheye images: The SVF can be calculated using analytical methods that derive the horizon limitation from geometric properties of the urban canyon (Johnson & Watson, 1984); vector-based methods that calculate the SVF from projected building envelopes on the sky using a 3D building database (Chen et al, 2012;Gál et al 2009;Gál & Unger, 2014;Unger, 2009); raster-based methods that use digital elevation models (DEMs) or DSMs to estimate SVFs based on pixel heights or shadow casting (Gál et al, 2009;Lindberg & Grimmond, 2011;Lindberg et al, 2008;Ratti, Baker, & Steemers, 2005;Zakšek, Oštir, & Kokalj, 2011), and photographic methods that use fisheye imagery of the upper hemisphere Chapman & Thornes, 2004;Grimmond, Potter, Zutter, & Souch, 2001;Holmer, Postgård, & Eriksson, 2001). The hemispheric horizon limitation is usually projected on a 2D plane to calculate the amount of visible sky in the scene.…”
Section: Sky View Factor Calculationmentioning
confidence: 99%
“…Finally, the software "SOLWEIG" [31] was used for the computation of the fourth SVF raster map. The software was developed as a tool for modeling the spatial variations of radiant fluxes and mean radiant temperature in complex urban settings, and in fact, the computation of the SVF is only an intermediate product.…”
Section: Svf Maps From Lidar Datamentioning
confidence: 99%