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Project Objectives

Land cover data. SWE distribution over northern hemisphere (Jan 10 2007). CO 2. CO 2. Example of snow cover area (SCA) product. Snow clearance date in northern hemisphere (0.25 deg EASE grid), 2008. Julian day from Jan 1. SNOWCARBO: Progress & Preliminary Achievements.

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Project Objectives

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  1. Land cover data SWE distribution over northern hemisphere (Jan 10 2007) CO2 CO2 Example of snow cover area (SCA) product Snow clearance date in northern hemisphere (0.25 deg EASE grid), 2008. Julian day from Jan 1. SNOWCARBO: Progress & Preliminary Achievements Introduction Preliminary Achievements • Establishment of the modeling system to the area of interest • Generation of satellite datasets (both FMI and SYKE) • Generation of dedicated land cover datasets in different scales • to test the sensitivity of the model and improve the characterization • of the land cover • Finding the correlation between field observations CO2 flux from • the towers and the satellite derived NDVI index • Field work in both Sodankylä-Pallas in-situ super site and in • dedicated field campaigns Photo: Kristin Böttcher Photo: Pekka Härmä Photo: Markus Törmä Project Objectives • Spectral measurements from a thin, melting snowpack were • carried out near Helsinki, for estimating errors in the • SCA- algorithm and for aiding the satellite time-series • Interpretation • Land cover data validation • Forest parameter estimation • Spectral measurements of vegetation Data Sets • AVHRR (Advanced Very High Resolution Radiometer) • European Centre for Medium-Range Weather Forecasts (ECMWF) snow depth observations (used as input for SWE product) • Weekly SWE (mm) • Snow melt onset (date, spring) • Snow clearance (date, spring) • Land Cover Data • MODIS (Moderate Resolution Imaging Spectroradiometer) Field Campaigns First results from CO2- flux estimations using JSBACH EC CO2 fluxes (dots) and JSBACH flux predictions (lines) for one grid cell 2003 • Temporal pattern from the JSBACH is good considering the following uncertainties: • Scaling of the fluxes (systematic shift) • Representativeness of the grid cell • ’Missing photosynthesis’ during summer months A comparison of SWE-output from REMO and SD-directly from Weather stations was made (partially under progress: different model versions) http://snowcarbo.fmi.fi

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