Pregled bibliografske jedinice broj: 1069840
Evolution and dynamics of the vertical temperature profile in an oligotrophic lake
Evolution and dynamics of the vertical temperature profile in an oligotrophic lake // Hydrology and earth system sciences, 24 (2020), 3394-3416 doi:10.5194/hess-24-3399-2020 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1069840 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Evolution and dynamics of the vertical
temperature profile in an
oligotrophic lake
Autori
Bencetić Klaić, Zvjezdana ; Babić, Karmen ; Orlić, Mirko
Izvornik
Hydrology and earth system sciences (1027-5606) 24
(2020);
3394-3416
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Plitvice Lakes ; internal seiche ; spectral analysis ; high-frequency baroclinic wave
Sažetak
In this study, the fine-scale responses of a stratified oligotrophic karstic lake (Kozjak Lake, Plitvice Lakes, Croatia ; the lake fetch is 2.3 km, and the maximum depth is 46 m) to atmospheric forcing on the lake surface are investigated. Lake temperatures measured at a resolution of 2 min at 15 depths ranging from 0.2 to 43 m, which were observed during the 6 July–5 November 2018 period, were analyzed. The results show thermocline deepening from 10m at the beginning of the observation period to 16m at the end of the observation period, where the latter depth corresponds to approximately one-third of the lake depth. The pycnocline followed the same pattern, except that the deepening occurred throughout the entire period approximately 1m above the thermocline. On average, thermocline deepening was 3– 4 cmd1, while the maximum deepening (12.5 cmd1) coincided with the occurrence of internal seiches. Furthermore, the results indicate three different types of forcings on the lake surface ; two of these forcings have diurnal periodicity – (1) continuous heat fluxes and (2) occasional periodic stronger winds – whereas forcing (3) corresponds to occasional nonperiodic stronger winds with steady along- basin directions. Continuous heat fluxes (1) produced forced diurnal oscillations in the lake temperature within the first 5m of the lake throughout the entire observation period. Noncontinuous periodic stronger winds (2) resulted in occasional forced diurnal oscillations in the lake temperatures at depths from approximately 7 to 20 m. Occasional strong and steady along-basin winds (3) triggered both baroclinic internal seiches with a principal period of 8.0 h and barotropic surface seiches with a principal period of 9 min. Lake currents produced by the surface seiches under realistic- topography conditions generated baroclinic oscillations of the thermocline region (at depths from 9 to 17 m) with periods corresponding to the period of surface seiches ( 9 min), which, to the best of our knowledge, has not been reported in previous lake studies.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika, Interdisciplinarne prirodne znanosti
POVEZANOST RADA
Projekti:
Ostalo-Ugovor br. 7989116 - Hidrodinamičko modeliranje sustava Plitvičkih jezera (Bencetić-Klaić, Zvjezdana; Rubinić, Josip; Kapelj, Sanja, Ostalo - Otvoreni natječaj Nacionalnog parka Plitvička jezera) ( CroRIS)
Hidrodinamičko modeliranje sustava Plitvičkih jezera (broj ugovora 7989/16)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus