Sentences with phrase «term rate of sea level»

The grey shading shows the uncertainty in the estimated long - term rate of sea level change (Section 6.4.3).

Not exact matches

The long - term average rate of sea - level rise in Hampton Roads is about one foot per century, but that pace has accelerated sharply recently, which makes it challenging to gauge future rates of change.
Several previous analyses of tide gauge records1, 2,3,4,5,6 — employing different methods to accommodate the spatial sparsity and temporal incompleteness of the data and to constrain the geometry of long - term sea - level change — have concluded that GMSL rose over the twentieth century at a mean rate of 1.6 to 1.9 millimetres per year.
The physics part is that to first order, you expect the rate of continental ice melt to increase with temperature, and also the rate at which heat penetrates into the ocean below the mixed layer (for the mixed layer indeed we use a term relating temperature to sea level, not its rate of rise).
Since the rate of the sea level raising is around 1 inch a year in sort of a «bursts» — the long - term will definitely be the one who poses less uncertainties, unlike the short - term.
While the near - term rate of sea - level rise remains uncertain, the long - term picture of rising seas in a warming world is crystal clear.
Schneider's approach to climate policy, comes up during a discussion of the enduring uncertainty surrounding the most consequential aspects of global warming, particularly the near - term rate at which sea levels will rise as ice sheets melt and seawater warms.
And they all assign large economic damage to sea - level rise — even though there is no observational evidence for an influence of short - term (decadal) temperature changes on the rate of rise of sea level.
Short period trends of acceleration in mean sea level after 1990 are evident at each site, although these are not abnormal or higher than other short - term rates measured throughout the historical record.»
Satellite data, which manifest the highest short - term rates of sea - level rise (but also great measurement uncertainties) belie your extravagant claims: the current rate is only 3.2 mm / year (https://climate.nasa.gov/vital-signs/sea-level/).
Over the 20th century, there was considerable decadal variation in the rate of sea - level rise but no long - term trend.
A: «Internal variability versus anthropogenic forcing on sea level and its components» B: «The rate of sea - level rise» C: «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» D: «Detection and attribution of global mean thermosteric sea level change» E: «Long - term sea level trends: Natural or anthropogenic?»
Specifically, smoothing sea - level data (adjusting for natural variability of ENSO) over the past century fits most closely with a 4th degree polynomial model, and there has very likely not been any slowing in the longer - term background rate of sea level rise over the period of the tropospheric «pause».
Mr Lord said long - term data gleaned from gauges in Sydney Harbour suggested sea levels were rising at the rate of about 1 mm per year.
4) Most of the post-1950s sea level rise is anthropogenic: «Internal Variability Versus Anthropogenic Forcing on Sea Level and Its Components» «The rate of sea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&raqsea level rise is anthropogenic: «Internal Variability Versus Anthropogenic Forcing on Sea Level and Its Components» «The rate of sea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&rlevel rise is anthropogenic: «Internal Variability Versus Anthropogenic Forcing on Sea Level and Its Components» «The rate of sea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&raqSea Level and Its Components» «The rate of sea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&rLevel and Its Components» «The rate of sea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&raqsea - level rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&rlevel rise» «Quantifying anthropogenic and natural contributions to thermosteric sea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&raqsea level rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&rlevel rise» «Detection and attribution of global mean thermosteric sea level change» «Long - term sea level trends: Natural or anthropogenic?&raqsea level change» «Long - term sea level trends: Natural or anthropogenic?&rlevel change» «Long - term sea level trends: Natural or anthropogenic?&raqsea level trends: Natural or anthropogenic?&rlevel trends: Natural or anthropogenic?»
The map of regional mean sea level trends provides an overview of variations in the rates of relative local mean sea level observed at long - term tide stations (based on a minimum of 30 years of data in order to account for long - term sea level variations and reduce errors in computing sea level trends based on monthly mean sea level).
«However, Fig. 15 and the associated uncertainties discussed in Section 3.4 show that long term estimates of time variable sea level acceleration in 203 year global reconstruction are significantly positive, which supports our previous finding (Jevrejeva et al., 2008a), that despite strong low frequency variability (larger than 60 years) the rate of sea level rise is increasing with time.»
«long term estimates of time variable sea level acceleration in 203 year global reconstruction are significantly positive, which supports our previous finding (Jevrejeva et al., 2008a), that despite strong low frequency variability (larger than 60 years) the rate of sea level rise is increasing with time.»
It will also confirm the accelerated rate of change for impacts such as sea - level rise, the steady retreat of Arctic sea ice and quickened melting of ice sheets and glaciers, as well as offer more detail on scenarios that will shape international negotiations over both short - term and long - term greenhouse gas emissions, including how long «business as usual» can be sustained without dangerous risk.
From what I understand about things like the viscosity of water & gravity, the actual rate of sea - level rise can't vary between locations on any long - term basis.
An ~ 100kyr periodicity in fast - spreading seafloor bathymetry, and relatively low present - day eruption rates, at a time of high sea - level and decreasing orbital eccentricity suggest a longer term sensitivity to sea - level and orbital variations associated with Milankovitch cycles.
Last August, I wrote about what that near - term worse case scenario might look like: Should its melt rate continue to trend above previous estimates, Antarctica may produce an extra foot of sea level rise by 2100, which would pose a threat to low - lying coastal areas worldwide.
Some further insights into longer term OHC variability can be inferred from this figure from the AR5 on rates of sea level rise:
a b c d e f g h i j k l m n o p q r s t u v w x y z