<time>Tue Apr 22 12:07:11 2014</time> <Solid> <id>6e359e22-e6d7-41d1-ba8c-91e0068704f7</id> <ValidatorMessage> <type>ERROR</type> <errorCode>210</errorCode> <errorType>NON_PLANAR_SURFACE</errorType> <shell>1</shell> <face>14</face> </ValidatorMessage> </Solid> <Solid> <id>59feffb1-604c-4032-b414-1d72f1d2371d</id> <ValidatorMessage> <type>ERROR</type> <errorCode>400</errorCode> <errorType>SHELLS_FACE_ADJACENT</errorType> <shell>2</shell> <face>3</face> </ValidatorMessage> </Solid> </val3dity> IDs of gml:Solid used link to specific surface where the problem is error type
b a c C 'JHVSF 5IF EBSUT JO UIF DFMM DPNQMFYFT JO 'JHVSF /PUF UIBU UIF EBSUT PG UIF SJHIU DVCF JO C XIFO WJFXFE BT JOEJWJEVBM TUBDLT BSF TJNJMBS UP UIF POFT JO 'JHVSF 5IF EBSUT PG UIF MFȈ CPY BSF IPXFWFS EJȊFSFOU UIPTF PO UIF MFȈ BMM JOWPMWF BO FYUSVTJPO BMPOH UIF JOUFSWBM ܐ EVF UP UIF GBDU UIBU UIFSF JT OP WFSUFY FEHF PS GBDFU FYUSVEFE UP 0O UIF PUIFS IBOE UIPTF JO UIF SJHIU EP IBWF B WFSUFY BOE BO FEHF BU CVU OPU B GBDFU BOE TUJMM CFMPOH UP UIF TBNF WPMVNF WBM BOE "MHPSJUIN CZ UIF FOE PG POF *G BO JOQVU EBSU JT EFOPUFE
LODs • Ways to get 3D models in multiple LODs: • Acquisition: Expensive • Generalisation: generalisation solutions not available • Procedural modelling: free
set of rules • Supplementing GIS data sets (-> synthetic data) • Suited for animations, gaming, movies, … • Example input: 2D footprints Müller et al. (2006). Procedural modeling of buildings. ACM Transactions on Graphics, 25(3), 614–623. http://doi.org/10.1145/1179352.1141931
multi-LOD generation and interior • Suited for multi-LOD experiments to compute the accuracy of each LOD 1.1 1.2 1.3 2.0 2.1 2.2 2.3 3 Level of detail 0.0 0.2 0.4 0.6 0.8 1.0 Normalised root mean square error and cost ✏1 ✏2 ✏3 Cost
the global solar irradiance on tilted surfaces. In Proceedings of EDPE 2013. Dubrovnik, Croatia, pp. 334–339. Global radiation = direct + diffuse + reflected
area, weather, …) • Many empirical models • Time-dependant—each day, each hour is different • Integrate the values over a year with 1h increments Perez, R. et al., 1990. Modeling daylight availability and irradiance components from direct and global irradiance. Solar Energy, 44(5), pp.271–289.
= tilt 40 deg towards south (180) • Surface B = vertical wall towards east (90, 90) • Surface H = horizontal surface (e.g. flat roof) • Dates: 1 Mar, 21 Jun • Location dependent, weather dependent
0 200 400 600 800 1000 Global solar radiation (W/m2) Clear-sky global solar radiation for Delft, the Netherlands A on 1 Mar B on 1 Mar H on 1 Mar A on 21 Jun B on 21 Jun H on 21 Jun