He received B.Sc. in Land Surveying Engineering (2000), and then the M.Sc. degree in Geodesy from K.N.Toosi University,Tehran, Iran in 2002, the Ph.D. degree from the Royal Institute of Technology (KTH), Stockholm, Sweden, in 2011. He promoted to Docent in Geodesy (2013). He is working as Professor at University of Gävle and Senior Researcher at KTH.
He is member of editorial board in Journal of Geodetic Science since 2013.
Except his academic activities he was project manager of railway and highway studies in different phases of construction of the projects in Metra Consulting Engineering Co. from 2001-2007 in Tehran-Iran.
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Sea level change will lead to changes in coastal impacts and increase environmental hazards. These changes are related to climate change that affects a lot of people’s daily life who live near coastal zone. Presently about 40% of the world's population lives within 100 kilometers of the coast and 25% of the global population lives in the near coastal zone within 100-meter elevation according to IPCC - Intergovernmental Panel on Climate Change reports. Climate change is one of the important issues today, due to its special weather conditions, which requires many studies to model the climate behavior.
For this purpose we use our knowledge of past and present observed sea level changes, as well as predicting the future sea level change using space geodesy techniques. Important factors for sea level change are the effects of ground ice changes (glaciers), land uplift due to glacial isostatic adjustment, seawater salinity, thermal expansion, and reduction of surface water storage (aquifers). We use satellite altimetry and gravimetry data (GRACE) and assimilate other in-situ data (tide gauges) as well as available hydrological and ocean circulation models to determine sea level change.
The GRACE has provided a valuable source of information about the time variable Earth’s gravity field, and more specifically water exchange as the main contributor to the Earth’s gravity field changes within decadal scales (mass component). Also, since 2004, the Argo project reached a global coverage of its floats measuring seawater temperature and salinity at different layers of ocean depth, which helps to model steric component of Global Mean Sea Level (GMSL). The following figures show the mass component, steric component and GMSL using different data centres. Generally the following relation is between GMSL and its components:
GMSL = Mass component (GRACE) + Steric Component (Argo data)
Our results show that GFZ products, applying Gaussian filter (300 km averaging radius) with a combination of JAMSTEC products (Argo data) is the best solution to determine the GMSL trend. The GMSL trend is 3.12 mm/year.
The main issues in this study were: