«This is an important finding because it highlights the role that the rapidly changing Greenland ice sheet plays in supplying nutrients to the Arctic Ocean,» observed Eran Hood of the University of Alaska Southeast in Juneau, who studies the meltwater
from coastal glaciers in Alaska, and was not involved in the new study.
Not exact matches
Whilst this is a small figure in actual terms, combined with the contribution
from other melting
glaciers around the world and expansion of the world's oceans, it will have an impact upon society through flooding of low - lying
coastal regions.»
Co-author Dr Ivan Haigh, lecturer in
coastal oceanography at the University of Southampton and also based at NOCS, adds: «Historical observations show a rising sea level
from about 1800 as sea water warmed up and melt water
from glaciers and ice fields flowed into the oceans.
Yes, it's part of the United States, English is spoken, and the dollar is used — but Alaska's wild
coastal plains, towering snow - capped mountains, and
glacier - rimmed fjords have a way of making you feel worlds away
from home.
If someone had told me that I could visit a single U.S state and see everything
from rugged
coastal landscapes and thick evergreen forests, to barren, fossil - strewn deserts, volcanoes and
glaciers, I probably wouldn't have believed them.
The same goes for the snouts of «outlet»
glaciers, where ice
from the interior funnels through gaps in
coastal mountain ranges, and where warming seawater has broken up clots of ice that can hold things up, like a logjam in a river.
Guardian and WAPO are reporting the study ways
coastal glaciers are melting
from below at faster rate than had been predicted.
As runoff
from melting
glaciers increases and warming seawater expands, sea level could rise as much as six feet, inundating low - lying
coastal areas and islands.
NASA's Oceans Melting Greenland (OMG) mission has released preliminary data on the heights of Greenland
coastal glaciers from its first airborne campaign in March 2016.
As you are aware sea level rise also has the effect of moving the grounding line proximally, which reduces the friction on the ice shelf or valley
glacier without reducing the gravitational force which is driving the ice
from the slopes beyond the
coastal plain.
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.
Thus the topography of the
coastal shelves and depth of submerged
glacier grounding points determines the impact of upwelled CDW and limits extreme basal melting to a relatively few locations as illustrated by the red and orange areas in the figure below (
from Depoorter 2013)..
See millions, billions, trillions traded for pigs, pokes, and lies... starving polar bears straight
from the sands of a sinking arctic... snarling snow leopards swept away by melting
glaciers... gasping Gurkhas in search of water...
coastal residents on stilts... climate grifters juggling semi-intelligent humans... grim reapers galloping the streets... massive throngs wandering aimlessly... You there in the back!
Unless global temperatures are stabilized, higher seas
from melting ice sheets and mountain
glaciers, combined with the heat - driven expansion of ocean water itself, will eventually lead to the displacement of millions of people as low - lying
coastal areas and island nations are inundated.
This change is likely to be most dramatic in Arctic
coastal waters, which are rapidly freshening due to the melting of ice on
glaciers and permafrost (McPhee et al. 2009), accelerating OA and Ωaragonite decline relative to the rates expected
from anthropogenic CO2 alone (Tank et al. 2012).
In his written testimony, Admiral McGinn cited a number of scenarios that could come to pass if we fail to address the climate problem: rising humanitarian crises and conflicts in Africa exacerbated by drought, food insecurity, and extreme weather; social conflict and northern migration in Latin American driven by food shortages and land degradation; millions of refugees driven northward by intense
coastal typhoon damage in Bangladesh; and external and internal unrest in Asia compounded by unreliable water supplies
from the shrinking Himalayan
glaciers.