Sentences with phrase «altimeter sea level trends»

Observed altimeter sea level trends (mm / year) during January 1993 to May 2017.
The spatial distribution of the altimeter sea level trends during 1993 - 2017 shows large - scale variations, with some regions such as the western tropical Pacific Ocean experiencing up to +8 mm / year.

Not exact matches

Throughout the altimeter era, it has been recognized that sea level rise is not constant but varies considerably about the background trend, with the largest of these departures coinciding with the warm and cold phases of the El Niño Southern Oscillation (ENSO) such as in 1997 — 1998 (Fig. 2).
Several other satellite altimeters have also been launched, and the data from these have been used to estimate global mean sea level trends since 1993.
Fig. 2 Global sea level from tide gauges (red) and satellite altimeter data (blue, with linear trend line).
«Trends and acceleration in global and regional sea levels since 1807» «Evaluation of the global mean sea level budget between 1993 and 2014» «Considerations for estimating the 20th century trend in global mean sea level» «New estimate of the current rate of sea level rise from a sea level budget approach» «Reassessment of 20th century global mean sea level rise» «The increasing rate of global mean sea - level rise during 1993 — 2014» «Unabated global mean sea - level rise over the satellite altimeter era» «An increase in the rate of global mean sea level rise since 2010»
Since 1993, an even higher sea level trend of about 2.8 mm / yr has been measured from the TOPEX / POSEIDON satellite altimeter.
The regional sea level trends are derived from a linear fit of the altimeter sea level maps for the global ocean.
Since 1992, sea level observations from satellite altimeters at millimeter accuracy reveal a global increase of ~ 3.2 mm year − 1 as a fairly linear trend (Fig. 4), although with two main blips corresponding to an enhanced rate of rise during the 1997 — 1998 El Niño and a brief slowdown in the 2007 — 2008 La Niña.
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