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1.	Sand, SJ, et al. (author) Benchmark calculations in risk assessment using continuous dose-response information: the influence of variance and the determination of a cut-off value 2003 In: Risk analysis : an official publication of the Society for Risk Analysis. - : Wiley. - 0272-4332. ; 23:5, s. 1059-1068 Journal article (peer-reviewed)
2.	Sand, S, et al. (author) Dose-response modeling and benchmark calculations from spontaneous behavior data on mice neonatally exposed to 2, 2 ' 4, 4 ', 5-pentabromodiphenyl ether 2004 In: TOXICOLOGY AND APPLIED PHARMACOLOGY. - 0041-008X. ; 197:3, s. 360-360 Conference paper (other academic/artistic)
3.	Sand, S, et al. (author) Dose-response modeling and benchmark calculations from spontaneous behavior data on mice neontally exposed to 2,2', 4,4',5-pentabromodiphenyl ether 2004 In: Toxicol Sci. ; 81:2, s. 491-501 Journal article (peer-reviewed)
4.	Semadeni Davies, Annette, et al. (author) Estimating latent heat over a melting arctic snow cover 2004 In: Nordic Hydrology. - 0029-1277. ; 35:3, s. 175-190 Journal article (peer-reviewed)abstract The latent heat flux over snow near Ny-Alesund, Spitsbergen, was investigated for the 1999 snowmelt season to assess different methods of modelling the flux. Snow evaporation had hitherto been estimated as the residual of plot water balance calculations and was subject to measurement errors: hence a modelling solution was sought to make use of existing data. Precipitation, snow depth and albedo we.-e measured daily. Runoff from the plots was recorded continuously. Wind speed, relative humidity and air temperature were measured at two levels (2 and 10 m) every 10 minutes; wind direction was noted hourly. Three models which simulate latent heat were assessed against evaporation and condensation measured by weighing several snow-filled containers each day. Two employ the bulk profile method (within the SNTHERM and CROCUS snowmelt models), while the third is the aerodynamic profile method (APM). Each follows tie measured evaporation until snow-free patches develop after which the APM predicts evaporation whereas the snowmelt models predict condensation. The effect of wind is also noted. A major conclusion of this work is that the complexity of the land surface/atmosphere interactions, particularly when the snow cover breaks up, precludes the use of simple models for determining latent heat.

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Type of publication: journal article (3); conference paper (1)

Type of content: peer-reviewed (3); other academic/artistic (1)

Author/Editor: von Rosen, D (3); Eriksson, P (2); FREDRIKSSON, A (2); Sand, S (2); Victorin, K (2); Viberg, H (2); show more...; Filipsson, AF (2); Semadeni Davies, Ann ... (1); Bruland, O (1); Kodama, Y. (1); Sand, K (1); Sand, SJ (1); Filipsson, A.F. (1); Marechal, D (1); show less...

University: Karolinska Institutet (2); Uppsala University (1); Lund University (1)

Language: English (4)

Research subject (UKÄ/SCB): Engineering and Technology (1)

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