air-sea fluxes over the ithaca region grbec, b. and matić, f. institute of oceanography and...
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![Page 1: Air-sea fluxes over the ITHACA region Grbec, B. and Matić, F. Institute of oceanography and fisheries - Split](https://reader036.vdocuments.net/reader036/viewer/2022062519/5697bf761a28abf838c81152/html5/thumbnails/1.jpg)
Air-sea fluxes over the ITHACA regionGrbec, B. and Matić, F.
Institute of oceanography and fisheries - Split
![Page 2: Air-sea fluxes over the ITHACA region Grbec, B. and Matić, F. Institute of oceanography and fisheries - Split](https://reader036.vdocuments.net/reader036/viewer/2022062519/5697bf761a28abf838c81152/html5/thumbnails/2.jpg)
)2()( ASHpAH TTVCcQ
)3()(622.0
)()(( ASEEAA
AsatSsatEEAE qqVCLp
TerTeVCLQ
)4(,)75.01()(4)05.04.0( 4.334 NTTTeTQ aSasatSL
Parameterization:
)1()cos(0 zbaIQ iiS
1) Matić, F.: Air sea interaction in the Brać, Hvar and Neretva channel, Master thesis, University of Zagreb, 2005.
2) May, P.: 1982, Climatological flux estimates in the Mediterranean Sea, Wind and wind stresses. Norda report 54.
3) , 4) Gill, A.: 1982, Atmosphere – ocean dynamics. Academic Press
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Meteorological station Split – Marjan;
SST station Split
• Qs: mean daily values calculated based on hourly values;
• Ql, QE, QC calculated based on daily averaged values of meteorological and SST values; all parameters except SST were measured hourly, SST at 07 and 14 h.
• Missing wind speed in June replaced by daily average from observations at 07, 14, 21 h. using relationship:
W = 0,836B **(3/2)
W is wind speed in m/s B is value
on the Beaufort-scale
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ITHACA period
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Monthly mean air temperature, precipitation, net heat and water flux (evaporation – precipitation) computed for Split-Marjan station for the period 1961-1990 and for 2003 and 2006. Vertical bars represent standard deviations for particular month.
ITHACA period vs 2003 and climatological mean
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• Surface fluxes will be calculated for all available meteorological and SST values on daily scale (daily average values);
• STATIONS: Split, Hvar, Komiža, Lastovo, Dubrovnik
• Based on ALADIN values surface fluxes will be calculated. For the SST field stations values, and/or satellite values will be calculated.
• AdHOCAdriatic sea Heat and water fluxes – Observation and Calculation.
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