WebJun 25, 2024 · Limited by the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GRACE-FO) measurement principle and sensors, the spatial resolution of mass flux solutions is about 2–3° in mid-latitudes at monthly intervals. To retrieve a mass flux solution in the Tibetan Plateau (TP) with better visual spatial … WebApr 5, 2024 · Antarctica is losing ice mass (melting) at an average rate of about 150 billion tons per year, and Greenland is losing about 270 billion tons per year, adding to sea … The animated map below shows the minimum size of the Arctic sea ice … This graph shows the change in global surface temperature compared to the … The first graph tracks the change in global sea level since 1993, as observed by … The current warming trend is different because it is clearly the result of human … Ice, which covers 10 percent of Earth's surface, is disappearing rapidly. Select a … Measuring Earth's Surface Mass and Water Changes GRACE Follow-On (GRACE … By accessing and using this information system, you acknowledge and consent … GREENLAND MASS VARIATION SINCE 2002 Data source: Ice mass …
Mass balance of the Greenland ice sheet from 1958 to …
WebGreenland and Antarctic ice mass variations on J 2 (2.0 and 1.7 × 10−11/year respectively). Their combined effect on the J 2 trend during the GRACE mission is 3.7 × 10 ... since 2002. However, when Greenland and Antarctica are added together the agreement with the SLR observations is good, as shown in Figure 3. Here, the secular effect of ... WebResearch based on observations from the Gravity Recovery and Climate Experiment (GRACE) satellites (2002-2024) and GRACE Follow-On (since 2024 - ) indicates that … solidworks cloud based
SVS - Antarctic Ice Mass Loss 2002-2024 - NASA
WebJun 28, 2024 · GrIS: (a) monthly and (b) seasonal mass variations estimated based on averaging the GRACE monthly solutions from four processing centers between April 2002 and June 2024 and after applying the ... WebAug 2, 2002 · Earth's mean tide-free dynamic oblateness (J 2) ≡ [C– (A +B)/2]/MR 2 = 1.082627 × 10 −3, where C > B ≥ Aare Earth's mean principal moments of inertia and M andR are the mean mass and radius, respectively.Satellite laser ranging (SLR) has yielded precise determination of the temporal variation in the low-degree spherical harmonic … WebSep 29, 2024 · Since its launch in 2002, ... We shall refer to this mode of ice-mass variations as the Greenland East-West Coastal Dipole (EWCD). With strong interannual undulation, EWCD's time history undergoes two … solidworks close sketch