Not exact matches
«Based on the UN climate panel's report on sea level rise, supplemented with an expert elicitation about the melting of the
ice sheets, for
example, how fast the
ice on Greenland and Antarctica will melt while considering the regional changes in the gravitational field and
land uplift, we have calculated how much the sea will rise in Northern Europe,» explains Aslak Grinsted.
To understand sea - level change means understanding not only the transfer of
land ice into the ocean, but also, for
example, how the gravitational field of the Earth changes as inconceivably large water volumes shift around the planet.
For
example, the agency is partnering with the Indian Space Research Organization to develop the NASA ISRO Synthetic Aperture Radar (NISAR) mission that will routinely provide systematic observations of Earth's
land and
ice - covered surfaces at least twice every 12 days, enabling greater scientific understanding of the dynamic processes that drive the Earth system and natural hazards, as well as providing actionable support for disaster response and recovery.
Along with tree rings and
ice cores, which offer a window into
land temperatures throughout Earth's history, these are all
examples of «climate proxies».
For
example, let just say that you slip on
ice and
land awkwardly on your hand and jam your shoulder.
There are also plenty of
examples where models have correctly suggested that different data sets were inconsistent (satellite vs. surface in the 1990s, tropical
ice age ocean temperatures vs.
land temperatures in the 1980s etc.) which were resolved in favor of the models.
Michael, the energy imbalance that results in the observed incidence of high temperature extremes and melting of
land ice, for
example, is not a perception.
Once it's trapped, it can go to a myriad of places -
land surface, oceans,
ice shelves,
ice sheets, glaciers for
example.»
For
example, let's say that evidence convinced me (in a way that I wasn't convinced previously) that all recent changes in
land surface temperatures and sea surface temperatures and atmospheric temperatures and deep sea temperatures and sea
ice extent and sea
ice volume and sea
ice density and moisture content in the air and cloud coverage and rainfall and measures of extreme weather were all directly tied to internal natural variability, and that I can now see that as the result of a statistical modeling of the trends as associated with natural phenomena.
A temperature rise of 5ºC would cause all
ice - free
land on the planet to experience dramatic changes in its eco-systems — for
example, tundra turning to forests and African grasslands to deserts.
Post-glacial rebound - The vertical movement of the
land and sea floor following the reduction of the load of an
ice mass, for
example, since the Last Glacial Maximum (21 ka).
For
example, as a result of
ice melting on
land, such as from glaciers and
ice sheets, as well as thermal expansion of the ocean, we have seen sea level rise 3.4 millimeters per year from 1993 - 2015, which puts coastal communities at risk of flooding and infrastructure damage.
For
example, although the sample size has been very small, studies of radio - collared seals in the Bering and Chukchi Seas observed those seals rarely hauled out at all, on
land or sea
ice, even when occupying
ice covered areas.
It has been noted for several decades that climate models tend to predict that Earth will become more sensitive to CO2 as, for
example, polar
ice melts, exposing open ocean and
land that absorb rather than reflect sunlight.
A well - known
example of this is the melting of
land - based
ice, which is contributing to sea - level rise (and adding to the effects of thermal expansion of the oceans), with implications for low - lying areas far beyond the polar and mountain regions where the melting is taking place.
For
example, with Étienne Berthier, of the Laboratoire d'Études en Géophysique et Océanographie Spatiales in Toulouse, I am writing a chapter on the Subantarctic for a book about GLIMS, the Global
Land Ice Measurements from Space initiative.
Scientific confidence of the occurrence of climate change include, for
example, that over at least the last 50 years there have been increases in the atmospheric concentration of CO2; increased nitrogen and soot (black carbon) deposition; changes in the surface heat and moisture fluxes over
land; increases in lower tropospheric and upper ocean temperatures and ocean heat content; the elevation of sea level; and a large decrease in summer Arctic sea
ice coverage and a modest increase in Antarctic sea
ice coverage.
For
example, one reason the Arctic has been melting faster in the summer of late is likely due to black carbon from Chinese coal plants that
land on the
ice and warm it faster.
I always assumed natural variability was due to semi-cyclical intra-system transfers of energy from, for
example, ocean to atmosphere or atmosphere to
land ice.
For
example,
land adjusts faster than ocean, and icy areas faster than non-icy due to extra
ice - albedo feedback.