AbstractGOCE (Gravity Field and Steady-State Ocean Circulation Explorer), the first Earth Explorer Core Mission in ESA’s Living Planet programme, has been launched on March 17th 2009. Employing an ultra-sensitive gradiometer on a very low altitude orbit in along-track drag-free condition, within about 2 years GOCE will provide a global model of the Earth’s gravity field and of the geoid to unprecedented spatial resolution and accuracy. Meanwhile, the requirement for monitoring the temporal variations of gravity with a spatial resolution similar to GOCE, but over much longer time periods than the lifetime of GOCE, is emerging. It is driven by the need to detect long-term periodicities and trends in geophysical phenomena that involve large mass redistributions (e.g. melting of the polar ice sheets, changes in continental water storage, etc.), which are extremely valuable for a better understanding of climate change. From a series of preparatory studies led by the European Space Agency (ESA) since 2003, it turned out that the most suitable technique for such a next-generation gravity mission is the so-called Low-Low Satellite-to-Satellite Tracking based on laser distance metrology. A first design of this mission and of its laser metrology system has been defined in the studies performed for ESA the team led by Thales Alenia Space Italia (TAS-I).


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    Title :

    The measurement of Earth’s gravity field after the GOCE mission


    Contributors:

    Published in:

    Acta Astronautica ; 67 , 7-8 ; 702-712


    Publication date :

    2010-06-16


    Size :

    11 pages




    Type of media :

    Article (Journal)


    Type of material :

    Electronic Resource


    Language :

    English





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