The implications of
these past changes in sea level for future rises are worrying, but uncertain.
«We think this will be useful for scientists trying to understand current and
past changes in sea level.»
Not exact matches
By validating model results against geological observations, the study indicates that
changes in runoff,
sea level and wave energy have profoundly affected the
past evolution of the Great Barrier Reef not only
in regard to reefs evolution but also sediment fate from source - to - sink.
Extraction of groundwater for irrigation and home and industrial use turns out to be an important missing piece of the puzzle
in estimates for
past and current
sea -
level changes and for projections of future rises
A working group known as PALSEA2 (Paleo constraints on
sea level rise) used
past records of local
change in sea level and converted them to a global mean
sea level by predicting how the surface of the Earth deforms due to
changes in ice - ocean loading of the crust, along with
changes in gravitational attraction on the ocean surface.
The
past climates that forced these
changes in ice volume and
sea level were reconstructed mainly from temperature - sensitive measurements
in ocean cores from around the globe, and from ice cores.
A new study by scientists at NASA's Jet Propulsion Laboratory (JPL)
in Pasadena, California, and the University of California, Irvine, shows that while ice sheets and glaciers continue to melt,
changes in weather and climate over the
past decade have caused Earth's continents to soak up and store an extra 3.2 trillion tons of water
in soils, lakes and underground aquifers, temporarily slowing the rate of
sea level rise by about 20 percent.
But the rapid retreat seen
in the
past 40 years means that
in the coming decades,
sea -
level rise will likely exceed this century's
sea -
level rise projections of 3 feet (90 centimeters) by 2100, issued by the Intergovernmental Panel on Climate
Change (IPCC), said Sridhar Anandakrishnan, a glaciologist at Pennsylvania State University, who was not involved
in the study.
This
sea level rise estimate is larger than that provided by the last IPCC report, but highlights the need for further research on ice sheet variablity and ice sheet response to climate
change, both now and
in the
past.
Returning to the quote from the interview, why should geologists disagree with AGW because they know how much
sea level has
changed in the
past?
Professor Kopp's research focuses on understanding uncertainty
in past and future climate
change, with major emphases on
sea -
level change and on the interactions between physical climate
change and the economy.
Some studies have attempted to estimate the statistical relationship between temperature and global
sea level seen
in the period for which tide gauge records exist (the last 2 - 3 centuries) and then, using geological reconstructions of
past temperature
changes, extrapolate backward («hindcast»)
past sea -
level changes.
However, there is a caveat: semi-empirical models are inherently calibrated to the historical experience, and potentially biased if the processes that will dominate
sea -
level change in the future are qualitatively different from those that drove it
in the
past.
How has global
sea level changed in the
past millennia?
That estimate was based
in part on the fact that
sea level is now rising 3.2 mm / yr (3.2 m / millennium)[57], an order of magnitude faster than the rate during the prior several thousand years, with rapid
change of ice sheet mass balance over the
past few decades [23] and Greenland and Antarctica now losing mass at accelerating rates [23]--[24].
Our framework links innovative approaches for (1) generating high - resolution, probabilistic projection of future climate and
sea -
level changes and (2) empirically identifying robust statistical relationships characterizing how humans have responded to
past climate variability and
past climate
change,
in order to (3) project how humans may respond to uncertain future
changes.
After over a year of sideways and downward movement from late 2015 through early 2017, the most recent NASA report shows that over the
past year an acceleration
in sea level rise has become visible on the NASA graph, even with just a quick glance (then again, while the long term trend is consistently upward, the annual trend is so variable, that it's likely foolish on my part to suggest a
change in trend based on the most recent periods of increase which have only been occurring for less than 12 months).
McGuire conducted a study that was published
in the journal Nature
in 1997 that looked at the connection between the
change in the rate of
sea level rise and volcanic activity
in the Mediterranean for the
past 80,000 years and found that when
sea level rose quickly, more volcanic eruptions occurred, increasing by a whopping 300 percent.
Robert Bindschadler of NASA and Tad Pfeffer at the University of Colorado, both glacier specialists, told me that they saw scant evidence that a yards - per - century rise
in seas could be produced from the ice sheets that currently cloak Greenland and West Antarctica, which are very different than what existed
in past periods of fast
sea -
level changes.
How has global
sea level changed in the
past millennia?
Past rates of
change, if used wisely, provide potential constraints of future projections, together with the many semi-empirical approaches to project future
sea -
level rise (e.g. Rahmstorf, 2007) which are typically greater
in magnitude than those from process based models.
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work
in time series analysis (an elegant use of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations
in the climate record and methods for smoothing temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike
in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence
in both climate model simulations and observational data for a 50 - 70 year oscillation
in the climate system; significantly Mike also published work with Kerry Emanuel
in 2006 showing that the AMO concept has been overstated as regards its role
in 20th century tropical Atlantic SST
changes, a finding recently reaffirmed by a study published
in Nature),
in showing how
changes in radiative forcing from volcanoes can affect ENSO,
in examining the role of solar variations
in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate
changes of
past centuries and phenomena such as Atlantic tropical cyclones and global
sea level, and even a bit of work
in atmospheric chemistry (an analysis of beryllium - 7 measurements).
In my briefings to the Association of Small Island States in Bali, the 41 Island Nations of the Caribbean, Pacific, and Indian Ocean (and later circulated to all member states), I pointed out that IPCC had seriously and systematically UNDERESTIMATED the extent of climate change, showing that the sensitivity of temperature and sea level to CO2 clearly shown by the past climate record in coral reefs, ice cores, and deep sea sediments is orders of magnitude higher than IPCC's model
In my briefings to the Association of Small Island States
in Bali, the 41 Island Nations of the Caribbean, Pacific, and Indian Ocean (and later circulated to all member states), I pointed out that IPCC had seriously and systematically UNDERESTIMATED the extent of climate change, showing that the sensitivity of temperature and sea level to CO2 clearly shown by the past climate record in coral reefs, ice cores, and deep sea sediments is orders of magnitude higher than IPCC's model
in Bali, the 41 Island Nations of the Caribbean, Pacific, and Indian Ocean (and later circulated to all member states), I pointed out that IPCC had seriously and systematically UNDERESTIMATED the extent of climate
change, showing that the sensitivity of temperature and
sea level to CO2 clearly shown by the
past climate record
in coral reefs, ice cores, and deep sea sediments is orders of magnitude higher than IPCC's model
in coral reefs, ice cores, and deep
sea sediments is orders of magnitude higher than IPCC's models.
In a more recent paper, our own Stefan Rahmstorf used a simple regression model to suggest that
sea level rise (SLR) could reach 0.5 to 1.4 meters above 1990
levels by 2100, but this did not consider individual processes like dynamic ice sheet
changes, being only based on how global
sea level has been linked to global warming over the
past 120 years.
Then he says: «We see the
level of
sea rise,
changing weather patterns,» «This year we have MORE [rain] than every year and for the last couple of weeks, the heavy rain falls throughout Vanuatu and it EXCEEDED what has happened
in the
past.»
I reached out to Pierrehumbert because he is one of many authors of «Consequences of twenty - first - century policy for multi-millennial climate and
sea -
level change,» an important new Nature Climate Change analysis reinforcing past work showing a very, very, very long impact (tens of millenniums) on the Earth system — climatic, coastal and otherwise — from the carbon dioxide buildup driven by the conversion, in our lifetimes, of vast amounts of fossil fuels into useful e
change,» an important new Nature Climate
Change analysis reinforcing past work showing a very, very, very long impact (tens of millenniums) on the Earth system — climatic, coastal and otherwise — from the carbon dioxide buildup driven by the conversion, in our lifetimes, of vast amounts of fossil fuels into useful e
Change analysis reinforcing
past work showing a very, very, very long impact (tens of millenniums) on the Earth system — climatic, coastal and otherwise — from the carbon dioxide buildup driven by the conversion,
in our lifetimes, of vast amounts of fossil fuels into useful energy.
Historically,
past sea level changes analyzed by NOAA have shown significant varations
in measurement.
This section focuses on global and regional
sea level variations, over time spans ranging from the last decade to the
past century; a brief discussion of
sea level change in previous centuries is given
in Section 5.5.2.4.
The scientists working on the IPCC assessments have carefully documented observed
changes in air temperature, ocean temperature, ice retreat, and
sea level rise since the
past century.
As
in the
past,
sea level change in the future will not be geographically uniform, with regional
sea level change varying within about ± 0.15 m of the mean
in a typical model projection.
Based on data from
past climate
changes, when
sea level rose to +5 — 9 m, including the occurrence of extreme storms — during a time when temperatures were less than 1 ◦ C warmer than today, experts warn of similar consequences
in coming decades.
No serious prediction can be made unless we have a good understanding of the
sea level changes today and
in the
past centuries.
A new study by NASA has indicated that climate
change has accelerated the global
sea level rise
in the
past few decades.
Sea levels have been increasing since the end of the last ice age, and the rate of
change is near the lowest
in the
past 15,000 years.
«Carbon choices determine US cities committed to futures below
sea level» «Economic impacts of climate
change in Europe:
sea -
level rise» «Future flood losses
in major coastal cities» «Forecasting the effects of accelerated
sea -
level rise on tidal marsh ecosystem services» «Coral islands defy
sea -
level rise over the
past century: Records from a central Pacific atoll»
Reconciling
past changes in Earth's rotation with 20th century global
sea -
level rise: Resolving Munk's enigma Jerry X. Mitrovica1, *, Carling C. Hay1, 2, Eric Morrow2, Robert E. Kopp2, 3, Mathieu Dumberry4, 5 and Sabine Stanley6 http://advances.sciencemag.org/content/1/11/e1500679.full
The study demonstrates that observation - based interpretations, highlighting the role of winds
in past regional
sea level variability, are not inconsistent with the dominance of AMOC - associated
changes in the 21st century.
A new study, published
in Journal of Geophysical Research - Oceans, helps clarify how
past and future coastal
sea level changes are related to local winds and large - scale ocean circulation.
According to the BAZ, recently Mörner has been at the Fiji Islands on multiple occasions
in order «to study coastal
changes and
sea level rise», and to take a first hand look at the «damage» that allegedly has occurred due to climate
change over the
past years.
Extending the
sea level record back over the entire century suggests that the high variability
in the rates of
sea level change observed over the
past 20 years were not particularly unusual.
Both the observations of mass balance and the estimates based on temperature
changes (Table 11.4) indicate a reduction of mass of glaciers and ice caps
in the recent
past, giving a contribution to global - average
sea level of 0.2 to 0.4 mm / yr over the last hundred years.
People have been forced to move
in the
past thanks to
changes in sea levels that affected Australia's coastline.
Here we present an analysis based on
sea -
level data from the altimetry record of the
past ~ 20 years that separates interannual natural variability
in sea level from the longer - term
change probably related to anthropogenic global warming.
«Here we present an analysis based on
sea -
level data from the altimetry record of the
past ~ 20 years that separates interannual natural variability
in sea level from the longer - term
change probably related to anthropogenic global warming... Our results confirm the need for quantifying and further removing from the climate records the short - term natural climate variability if one wants to extract the global warming signal.»
«The study findings may seem counter-intuitive, given that (the)
sea level has been rising
in the region over the
past half century, but the dominant mode of
change over that time on Tuvalu has been expansion, not erosion.»
«You need to understand why
sea level has
changed (both
in the
past century and the
past 20,000 years) and apply that knowledge to what will happen by the year 2100.»
Even while identifying some of the observed
change in climatic behaviour, such as a 0.4 C increase
in surface temperature over the
past century, or about 1 mm per year
sea level rise
in Northern Indian Ocean, or wider variation
in rainfall patterns, the document notes that no firm link between the do...
The findings of a study by AER scientists were referenced
in Chapter 13 as an example of geodynamic surface - loading models that can be used to describe the
past and present
changes in sea level caused by the redistribution of surface mass.
(Reuters)--
Sea level rise
in the
past two decades has accelerated faster than previously thought
in a sign of climate
change threatening coasts from Florida to Bangladesh, a study said on Wednesday.
This Section places particular emphasis on current knowledge of
past changes in key climate variables: temperature, precipitation and atmospheric moisture, snow cover, extent of land and
sea ice,
sea level, patterns
in atmospheric and oceanic circulation, extreme weather and climate events, and overall features of the climate variability.