Although gravity is often assumed to be a constant, it actually varies depending where you are on Earth. Gravity is weaker near the equator due to the centrifugal forces of the planet spinning through space, it is lower at locations further from the Earth\u2019s core like on mountain peaks. There\u2019s also the fact the Earth isn\u2019t a perfect sphere, nor uniformly dense.\n(The lowest gravitational acceleration on the planet has been measured at Mount Nevado Huascaran in Peru while the highest is at the surface of the Arctic Ocean)\n \nGravity even changes from month to month due to the enormous mass of the oceans moving around the Earth\u2019s surface.\n \nThat\u2019s a major headache for civil engineering projects like tunnels and skyscrapers, which need the local gravity for precision measurements. It also makes it difficult for scientists trying to gain a picture of sea level changes and how these relate to water tables, ice sheets and climate change.\n \nIn 2002, NASA launched the Gravity Recovery and Climate Experiment(GRACE) mission, sending two identical car-sized satellites to space. A microwave ranging system monitored the distance between them to within a micron, allowing scientists to map gravity by measuring tiny changes in distance between the two satellites as each of them speeds up and slows down in response to gravitational force.\n \nThose satellites stopped working last year. This morning two replacement satellites \u2013 the GRACE Follow-On (FO) mission \u2013 launched into space from Vandenberg Airforce Base in California aboard a Space X Falcon 9 rocket.\n \n\nInstead of microwave ranging systems, these satellites carry a laser based system developed by scientists from the Australian National University (ANU). The laser system is able to measure changes in their separation to the nearest micron \u2013 a thousandth of a millimetre \u2013 a tenth of the width of a human hair.\nThe GRACE FO satellites were developed by American, German and Australian scientists, with the Australian team \u2013 funded by a $4.7 million Australian Space Research Grant \u2013 led by ANU\u2019s Professor Daniel Shaddock.\n \nCredit: Airbus DS GmbH\/A. Ruttloff\n\u201cThis will be the first mission that shoots laser beams between space craft, to improve the measurement by a factor of 20. This is the same technology that we\u2019re developing for the multi-billion dollar gravitational wave detector mission we\u2019ll launch in around a decade,\u201d Shaddock said.\n\u201cThis can tell us about changes in sea level and it can give us a complete map of the melting of ice in Greenland or Antarctica, but it can also tell us how the ground water changes in the Murray Darling Basin from one month to the next,\u201d he added.\n \n\nThe satellites \u2013 part of a US-German led mission \u2013 fly around 220 kilometres apart after they deployed into orbit at around 6am this morning.\n\u201cAn increase in mass on Earth will make gravity stronger, which will cause one satellite to accelerate, which changes the distance between them,\u201d Shaddock said. \u201cThere are already other missions planned around Mars and other planets to map their mass.\u201d\n \nNASA\/JPL-Caltech\nThe university has also developed software to analyse the data from the mission. The ANU Research School of Earth Sciences\u2019 will use the data to estimate the melting of polar ice sheets, increases in ocean mass and hydrological changes across Australia and the world.\nThe school\u2019s Dr Paul Tregoning said knowing how fast the ice sheets of Greenland and Antarctica were melting was critical for assessing the impacts of climate change on Earth.\n \n\u201cGRACE FO measurements will quantify what is actually happening, providing clear evidence of the impacts of climate change,\u201d Tregoning said.