Mass balance and mass loss acceleration of the Greenland ice sheet (2002 - 2011) from GRACE gravity data

• Published in: Journal of Geodetic Science
• Main Authors: Joodaki, G., Nahavandchi, H.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Walter de Gruyter GmbH 2012
• Subjects: Applied Mathematics; Earth and Planetary Sciences (miscellaneous); Computers in Earth Sciences; Geophysics; Astronomy and Astrophysics; Greenland; Ice Sheet
• Online Access: http://dx.doi.org/10.2478/v10156-011-0032-9; https://www.degruyter.com/view/journals/jogs/2/2/article-p156.xml; https://www.degruyter.com/downloadpdf/journals/jogs/2/2/article-p156.xml

Mass balance and mass loss acceleration of the Greenland ice sheet (2002 - 2011) from GRACE gravity data We examine the magnitude and acceleration of the Greenland ice sheet mass loss between 2002 and 2011. We use monthly observations of time-variable gravity from the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission. The Greenland mass loss during this time period is not a constant, but accelerating with time. We have used a quadratic trend in addition to a linear trend, which is usually applied to the GRACE monthly time series of ice mass changes, to show that it better represents GRACE observations. Results of computations provide a mass decrease of -166±20 Gigatonne per year (Gt/yr) by using a linear trend and -111±21 Gt/yr by fitting a quadratic trend to the monthly time series. Quadratic fitting shows that the mass loss increases from -121 Gt/yr in 2002 - 2003 to -210 Gt/yr in 2006 - 2007 and -271 Gt/yr in 2010 - 2011 with an acceleration of -32±6 Gt/yr 2 in 2002 - 2011. This implies that the Greenland ice sheet contribution to sea level rise becomes larger with time. Contrary to recent studies, we use a non-isotropic filter whose degree of smoothing corresponds to a Gaussian filter with a radius of 340 km. Stripping effects in the GRACE data, C 20 effect, and leakage effects are applied.