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| 2. |
- Rahm, Lars, 1948-, et al.
(författare)
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Heat balance in a shallow cove
- 1986
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Ingår i: Estuarine, Coastal and Shelf Science. - 0272-7714 .- 1096-0015. ; 23, s. 705-724
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Tidskriftsartikel (refereegranskat)
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| 3. |
- Rahm, Lars, 1948-
(författare)
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A note on some hydrographic properties of the Eastern Gotland Basin
- 1988
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Ingår i: Beiträge fur Meereskunde. - 0067-5148. ; 58, s. 47-58
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Tidskriftsartikel (refereegranskat)abstract
- Mean values of salinity, temperature and oxygen concentrations are determined for the hydrographic station Gotland Deep (BY15) by field data obtained from the Fishery Board of Sweden for the period 1957-1982. These estimates are compared with the corresponding values of the entire basin, the Eastern Gotland Basin, which are attained by a volume-weighted procedure based on eight hydrographic stations in this area.
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| 4. |
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| 5. |
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| 6. |
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| 7. |
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| 8. |
- Rahm, Lars, 1948-
(författare)
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On the diffusive salt flux of the Baltic proper
- 1985
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Ingår i: Tellus. Series A, Dynamic meteorology and oceanography. - : Stockholm University Press. - 0280-6495 .- 1600-0870. ; 37A:1, s. 87-96
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Tidskriftsartikel (refereegranskat)abstract
- Turbulent cross-isohaline salt fluxes in the Baltic proper are studied with the aid of a one-dimensional “advection-diffusion” model. The theoretical framework of this model has been outlined by Walin. It is based on time-averaged T-S data from both the inflow and interior regions of the Baltic. The results obtained are in good agreement with some estimates of the mixing properties in the region. Based on this investigation, a discussion of the properties of the model and its applicability to a real estuarine system is performed.
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| 9. |
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| 10. |
- Rahm, Lars, 1948-
(författare)
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On the thermal adjustment of an almost-enclosed fluid region with through-flow
- 1986
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Ingår i: International Journal of Heat and Mass Transfer. - : Elsevier BV. - 0017-9310 .- 1879-2189. ; 29:10, s. 1479-1485
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Tidskriftsartikel (refereegranskat)abstract
- The dynamics of a heat-up process in a horizontally enclosed fluid region, with an imposed through-flow and subject to weak thermal forcing, is investigated. Based on a boundary layer approach, a simple one-dimensional model for the interior fluid region is derived. The predicted response of the temperature field agrees well with numerical solutions of the corresponding undegenerate one-dimensional problem. The analytical results are in reasonably close agreement with numerical results presented in a companion paper by Hyun and Hyun (Int. J. Heat Mass Transfer 29, 1487–1493 (1986)).
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