Pregled bibliografske jedinice broj: 236221
Radiative destabilization of the nocturnal stable atmospheric boundary-layer over the desert
Radiative destabilization of the nocturnal stable atmospheric boundary-layer over the desert // Boundary-Layer Meteorology, 61 (1992), 1-2; 1-12 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 236221 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Radiative destabilization of the nocturnal stable atmospheric boundary-layer over the desert
Autori
Grisogono, Branko ; Keislar, R. E.
Izvornik
Boundary-Layer Meteorology (0006-8314) 61
(1992), 1-2;
1-12
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
wave
Sažetak
Radiative destabilization of the nocturnal stable atmospheric boundary layer (NSABL) over homogeneous desert terrain is predicted by an analytical model based on a modified diffusion equation. The model applies late at night under calm, dry conditions when long-wave radiative transfer dominates the NSABL evolution. A three-layer structure for the NSABL is proposed: a shear sub-layer closest to the surface, a radiative sub-layer which contains the inversion top, and a coupling sub-layer which matches the NSABL with the residual layer aloft. A sub-sub-layer called the nocturnal internal boundary layer (NIBL) is nested within the radiative sub-layer and comprises the temperature maximum. The model can explain: (1) maximum cooling in the NIBL, (2) deepening of the NIBL, (3) radiative destabilization of the NSABL, and (4) possible surface warming before sunrise. An example from the Mohave Desert, USA is presented, and the observed temperature profile compares favorably with the model solution.
Izvorni jezik
Engleski
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus