Air-sea fluxes over the ITHACA region Grbec, B. and Matić, F. Institute of oceanography and fisheries - Split.

Slides:

Advertisements

Similar presentations

Basics of numerical oceanic and coupled modelling Antonio Navarra Istituto Nazionale di Geofisica e Vulcanologia Italy Simon Mason Scripps Institution.

Advertisements

Meteorologisk Institutt met.no OPNet, Oslo, May 2011 Do we need fine scale ocean prediction ?!... and if so, do we have the right tools ? Lars-Anders Breivik.

1 Preliminary Simulation of the Regional Coupled Atmosphere-Ocean Model in the Southern California Coastal Regions (Santa Ana Winds and Air-Sea Interaction)

Circulation in the atmosphere

Schematic diagram of basin inflows and outflows forconservation of volume discussion. TALLEY.

THE BEST ANALYZED AIR- SEA FLUXES FOR SEASONAL FORECASTING 2.12 Glenn H. White, W. Wang, S. Saha, D. Behringer, S. Nadiga and H.-L. Pan Global Climate.

Indirect Determination of Surface Heat Fluxes in the Northern Adriatic Sea via the Heat Budget R. P. Signell, A. Russo, J. W. Book, S. Carniel, J. Chiggiato,

1 Variability of sea surface temperature diurnal warming Carol Anne Clayson Florida State University Geophysical Fluid Dynamics Institute SSTST Meeting.

Using Scatterometers and Radiometers to Estimate Ocean Wind Speeds and Latent Heat Flux Presented by: Brad Matichak April 30, 2008 Based on an article.

Chapter 6: Global Fluxes and The Deep Circulation Heat Budget Conservation of Salt Oceanic Water Masses Oceanic Mixing Temperature - Salinity Diagrams.

Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.

Forecasting Ocean Waves Problem: Given observed or expected weather, what will be the sea state? Ships are sunk not by winds, but by waves!

The Atmosphere: Part 5: Large-scale motions Composition / Structure Radiative transfer Vertical and latitudinal heat transport Atmospheric circulation.

Coupled GCM The Challenges of linking the atmosphere and ocean circulation.

Why We Care or Why We Go to Sea.

Calculating the amount of atmospheric carbon dioxide absorbed by the oceans Helen Kettle & Chris Merchant School of GeoSciences, University of Edinburgh,

XBT measurements in the Southern Adriatic Mira Morović, Vlado Dadić, Frano Matić, Branka Grbec, Stipe Muslim Institute of Oceanography and Fisheries,

The speaker took this picture on 11 December, 2012 over the ocean near Japan. 2014/07/29 AOGS 11th Annual Meeting in Sapporo.

Oceanography 569 Oceanographic Data Analysis Laboratory Kathie Kelly Applied Physics Laboratory 515 Ben Hall IR Bldg class web site: faculty.washington.edu/kellyapl/classes/ocean569_.

Thermohaline and optical properties of the Drvenik-Hvar-Pelješac area Branka Grbec 1 (thermohaline), M ira Morović 1* (optical), Frano Matić 1,

Dataset Development within the Surface Processes Group David I. Berry and Elizabeth C. Kent.

SEADATANET Kick-Off Meeting Heraklion 8-10 June 2006 National Institute of Geophisics and Volcanology, Italy (INGV) SEADATANET Joint Reasearch Activities.

Sara Vieira Committee members: Dr. Peter Webster

Downscaling Future Climate Scenarios for the North Sea 2006 ROMS/TOMS Workshop, Alcalá de Henares, 6-8 November Bjørn Ådlandsvik Institute of Marine Research.

P. N. Vinayachandran Centre for Atmospheric and Oceanic Sciences (CAOS) Indian Institute of Science (IISc) Bangalore Summer.

Latest results in verification over Poland Katarzyna Starosta, Joanna Linkowska Institute of Meteorology and Water Management, Warsaw 9th COSMO General.

Meteorological Data Analysis Urban, Regional Modeling and Analysis Section Division of Air Resources New York State Department of Environmental Conservation.

Regional Air-Sea Interactions in Eastern Pacific 6th International RSM Workshop Palisades, New York July 11-15, th International RSM Workshop Palisades,

Why We Care or Why We Go to Sea.

Dispersion conditions in complex terrain - a case study of the January 2010 air pollution episode in Norway Viel Ødegaard Norwegian Meteorological.

Weather Vs. Climate Weather: atmospheric conditions in a particular location over a short period of time (a day to a week)

Physics - Dynamics Interface The 14th ALADIN Workshop Innsbruck, 1-4 June 2004 Martina Tudor Meteorological and Hydrological Service, Grič 3, HR

Bulk Parameterizations for Wind Stress and Heat Fluxes (Chou 1993; Chou et al. 2003) Outlines: Eddy correlation (covariance) method Eddy correlation (covariance)

An evaluation of satellite derived air-sea fluxes through use in ocean general circulation model Vijay K Agarwal, Rashmi Sharma, Neeraj Agarwal Meteorology.

Investigation of Mixed Layer Depth in the Southern Ocean by using a 1-D mixed layer model Chin-Ying Chien & Kevin Speer Geophysical Fluid Dynamics Institute,

Graduate Course: Advanced Remote Sensing Data Analysis and Application A COMPARISON OF LATENT HEAT FLUXES OVER GLOBAL OCEANS FOR FOUR FLUX PRODUCTS Shu-Hsien.

Global Ocean Circulation (2) 1.Wind-driven gyre-scale circulation of the surface ocean and upper thermocline 2.Global heat and freshwater water transport,

The Character of North Atlantic Subtropical Mode Water Potential Vorticity Forcing Otmar Olsina, William Dewar Dept. of Oceanography, Florida State University.

Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.

Class 8. Oceans Figure: Ocean Depth (mean = 3.7 km)

Ocean Surface heat fluxes

1 Development of a Regional Coupled Ocean-Atmosphere Model Hyodae Seo, Arthur J. Miller, John O. Roads, and Masao Kanamitsu Scripps Institution of Oceanography.

Contributions to SST Anomalies in the Atlantic Ocean [Ocean Control of Air-Sea Heat Fluxes] Kathie Kelly Suzanne Dickinson and LuAnne Thompson University.

Numerical Investigation of Air- Sea Interactions During Winter Extratropical Storms Presented by Jill Nelson M.S. Marine Science Candidate Graduate Research.

COSMO General Meeting Zurich, 2005 Institute of Meteorology and Water Management Warsaw, Poland- 1 - Simple Kalman filter – a “smoking gun” of shortages.

Ground-based energy flux measurements for calibration of the Advanced Thermal and Land Application Sensor (ATLAS) 1 Eric W. Harmsen and Richard Díaz Román,

A step toward operational use of AMSR-E horizontal polarized radiance in JMA global data assimilation system Masahiro Kazumori Numerical Prediction Division.

Interannual to decadal variability of circulation in the northern Japan/East Sea, Dmitry Stepanov 1, Victoriia Stepanova 1 and Anatoly Gusev.

The Mediterranean Forecasting INGV-Bologna.

SPURS Synthesis Research Objectives: Budget calculations Resolve important terms of the freshwater and heat budgets of the upper 1000 m on temporal scales.

HIRLAM coupled to the ocean wave model WAM. Verification and improvements in forecast skill. Morten Ødegaard Køltzow, Øyvind Sætra and Ana Carrasco. The.

THE BC SHELF ROMS MODEL THE BC SHELF ROMS MODEL Diane Masson, Isaak Fain, Mike Foreman Institute of Ocean Sciences Fisheries and Oceans, Canada The Canadian.

Modelling activities at Institute of Oceanography and Fisheries (IOF), Split within ADRICOSM-EXT project Gordana Beg Paklar Institute of Oceanography and.

A New Climatology of Surface Energy Budget for the Detection and Modeling of Water and Energy Cycle Change across Sub-seasonal to Decadal Timescales Jingfeng.

High-resolution operational NWP for forecasting meteotsunamis

Status and Outlook Evaluating CFSR Air-Sea Heat, Freshwater, and Momentum Fluxes in the context of the Global Energy and Freshwater Budgets PI: Lisan.

High-resolution operational NWP for forecasting meteotsunamis

XBT measurements in the Southern Adriatic

Recent changes in the ALADIN operational suite

Intraseasonal latent heat flux based on satellite observations

Mark A. Bourassa and Qi Shi

Branches of Oceanography

The HOAPS-3 climatology

Forecasting Ocean Waves

Heat Transport by the Atmosphere and ocean

Comparison of Aircraft Observations With Surface Observations from

Assessment of the Surface Mixed Layer Using Glider and Buoy Data

Joint Proposal to WGOMD for a community ocean model experiment

Compare and Contrast of cloud base height data

CHAPTER 3 LESSON 2 SYSTEM INTERACTIONS.

Presentation transcript:

Air-sea fluxes over the ITHACA region Grbec, B. and Matić, F. Institute of oceanography and fisheries - Split

Parameterization: 1)Matić, F.: Air sea interaction in the Brać, Hvar and Neretva channel, Master thesis, University of Zagreb, )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

Meteorological station Split – Marjan; SST station Split Qs: mean daily values calculated based on hourly values; Q l, Q E, Q C 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

ITHACA period

Monthly mean air temperature, precipitation, net heat and water flux (evaporation – precipitation) computed for Split-Marjan station for the period and for 2003 and Vertical bars represent standard deviations for particular month. ITHACA period vs 2003 and climatological mean

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. AdHOC Adriatic sea Heat and water fluxes – Observation and Calculation. NEXT