Sentences with phrase «other land ice»

So is melting of glaciers and other land ice that contribute to rising sea levels.

Not exact matches

So there's been a lot of great work by NASA and other organizations in early exploration of Mars and understanding... what Mars is like, where could we land, what's the composition of the atmosphere, where is there water — water ice, I should say — and so we need to go from these early exploration missions to actually building a city.
His warning is either directly communicated by wireless to land or relayed from ship to ship until it eventually reaches the United States Hydrographic Office at Washington, D. C. Wrecks, derelicts, ice, and other obstructions to navigation are promptly reported.
On the other hand, wind turbines also have a habit of icing up and, occasionally, throwing ice under those kinds of frost conditions, says Kathryn McCullough, whose family owns a wind farm and an agricultural farm on the same land in Oregon.
In addition to the atmosphere, models must also include other key earthly elements, such as the ocean, land masses and even sea ice.
One of them broke apart at an altitude of about 18 kilometres, the other sailed on to eventually land in Lake Chebarkul, leaving a 7 - metre - wide hole in the ice.
Lake Whillans had likely not seen the light of day for hundreds of thousands of years, but Tulacyzk and the others who landed that day intended to see what was under the ice.
Wind and other problems caused the 6.1 - kilogram Puma crash landings on ice and water during the mission, although NOAA and AeroVironment kept fixing the drones and did manage one run of about 46 kilometers, according to a report on the KQED Science Web site.
If all the ice in Greenland were to melt in coming decades (an unlikely scenario), it would raise sea levels by seven meters (more than 20 feet)-- enough to swamp New Orleans, Florida's coast, Bangladesh and the Netherlands, among other low - lying lands.
Other experts, though, say thinning ice sheets on land and calving ice shelves on the sea are reasons for alarm.
Exactly how sea - ice decline might affect species interactions in this and other types of food webs on land in the Arctic is a question that deserves greater attention,» Post said.
So, if Larsen C ultimately breaks up, researchers are concerned that could be a sign that other ice shelves holding back a large amount of land ice could cause oceans to rise.
Leaving aside the collapse of the Larsen - B ice shelf and other ice shelves in Antarctica, is it too simplistic to expect that dramatic changes should be anticipated first in the Arctic because it is sea covered by a few meters of sea ice and therefore more susceptible to change, in comparison to Antarctica (which is obviously land covered by glacial ice up to several kilometers thick in places)?
«Other glaciers» includes all other land - ice souOther glaciers» includes all other land - ice souother land - ice sources.
By combining the ocean heating rates, TOA observations (figure 4) and other energy storage terms (land, atmosphere warming and ice melt), the authors calculated Earth's energy imbalance from January 2001 - December 2010 to be 0.5 (± 0.43) W / m2.
development of a regional scale earth system model that includes coupling WRF with other earth system components such as ocean, sea ice, land surface hydrology, ecosystem, and chemistry; and
Land - based ice, on the other hand, is much more troublesome.
The Gravity Recovery and Climate Experiment (GRACE), the satellites tasked with measuring the mass changes in Greenland and other icy landscapes around the world, has a hard time time seeing the difference between rising land and ice.
«This deposit is probably more accessible than most water ice on Mars, because it is at a relatively low latitude and it lies in a flat, smooth area where landing a spacecraft would be easier than at some of the other areas with buried ice,» researcher Jack Holt of the University of Texas said in a statement.
Related Reviews: New: DreamWorks Holiday Classics • Arthur Christmas • Pixar Short Films Collection, Volume 2 • The Muppet Christmas Carol Also New: The Santa Clause (3 - Movie Collection) • Brave • Hot in Cleveland: Season Three • Cinderella • Bugs Bunny Superstar Phineas and Ferb: A Very Perry Christmas • Ice Age: A Mammoth Christmas Special • Dragons: Gift of the Night Fury & Book of Dragons Mickey's Christmas Carol • A Charlie Brown Christmas • A Chipmunk Christmas •» T was the Night Before Christmas Mickey's Magical Christmas • Beauty and the Beast: The Enchanted Christmas • A Muppets Christmas: Letters to Santa I Want a Dog for Christmas, Charlie Brown • Yogi Bear's All - Star Comedy Christmas Caper • A Miser Brothers» Christmas Elf • A Christmas Carol (2009) • Santa Claus: The Movie • The Christmas Star • The Nightmare Before Christmas • One Magic Christmas Disney Computer Animation: Bolt • Tangled • Chicken Little • Mickey Mouse Clubhouse: Mickey Saves Santa and Other Mouseketales The Prep & Landing Voice Cast: A Bug's Life • NewsRadio: The Complete Series • Scrubs: The Complete First Season
Like other sea - holes or «vertical caves,» the Great Blue Hole in Belize's Lighthouse Reef actually formed on dry land, during a past ice age when the sea level was a lot lower than it is today.
- as Captain Olimar is making his way home, an asteroid onslaught forces him to land on a nearby planet - Sparklium is the fuel for Olimar's Dolphin III ship - with the ship's fuel depleted, you have to find items on this planet which can be turned into fuel - collect everything from seeds to large scale treasures - you need 30,000 Sparklium to make your way home - you are eventually required to find a lost ship part at the end of the game - levels are more linear and puzzle based, and include specific goals / goodies to collect - move Captain Olimar with the Circle Pad, while all other interactions use the touchscreen - blow your whistle, throw Pikmin and also touch certain objects - worlds are called Sectors, with six areas altogether - find all the treasure and look for new passageways to complete a sector 100 % - passageways can grant you access to secret spots or additional levels highlighted with the letter X - the first world is called Brilliant Garden, which has lush forest environments - Yellow Pikmin can easily reach the upper screen, where you can sometimes collect goodies and pull down vines - there's a level where you use yellow Pikmin as a source to connect two wires - connecting the wires lets you see enemies and platforms that were hidden in the shadows - Winged Pikmin can be flung at high speeds, and they can pick up Olimar and help him descend down into new areas - in a later level, you need to use red Pikmin to stomp out fire and clear the way for you - Rock Pikmin are the strongest ones of the bunch and can break crystals - blue Pikmin can swim and fight well underwater - the maximum amount of Pikmin you can have in a stage is 20 - blow your whistle to call over the correct Pikmin for a task or puzzle - Ravaged Rustworks offers a unique industrial environment where you climb on pipes - Loney Tower has you climbing to the top of a tower without any help of Pikmin, and instead use pipes and Olimar's jetpack - Valley of the Breeze, found in the Leafswirl Lagoon sector, relies complete on Winged Pikmin - Barriers of Flame is in the Sweltering Parchlands sector - here you «lll be forced to improvise with Yellow and Rock Pikmin to get around fire - every world ends with a boss stage - one boss fight puts you up against a Fiery Blowhog, where you use Red Pikmin to pick up / feed bombs to the boss - beating bosses gives you treasures worth 1,000 Sparklium each - supports amiibo in the Splatoon, Super Mario and Animal Crossing lines - amiibo can be scanned in to grant you access to secret spots - these are one room puzzle challenges where you collect a statue - these bonus rooms will also get you 200 Sparklium every time - you are limited by how many amiibo you can summon to each secret spot - one of the treasures you will find is an NES cartridge for Ice Climbers, which carries the name «Revenge Fantasy».
The desert, ice, and sky - themed lands in particular would become staples (with the former most often found in the second world) of the series, especially when Nintendo decided to do more 2D platformers beginning with New Super Mario Bros. on the Nintendo DS in 2006, while a variety of other styles would emerge over the years as well.
Leaving aside the collapse of the Larsen - B ice shelf and other ice shelves in Antarctica, is it too simplistic to expect that dramatic changes should be anticipated first in the Arctic because it is sea covered by a few meters of sea ice and therefore more susceptible to change, in comparison to Antarctica (which is obviously land covered by glacial ice up to several kilometers thick in places)?
Other factors would include: — albedo shifts (both from ice > water, and from increased biological activity, and from edge melt revealing more land, and from more old dust coming to the surface...); — direct effect of CO2 on ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; — melting of sea ice shelf increasing mobility of glaciers; — sea water getting under parts of the ice sheets where the base is below sea level; — melt water lubricating the ice sheet base; — changes in ocean currents -LRB-?)
Her work showed that polar bears, while best known for their life at sea or on sea ice pursuing seals, have been able, at least in some circumstances, to gain significant nutrition on land as well, scarfing down geese and goose eggs, grasses and other fare when sea ice is in retreat.
The IPCC Fourth Assessment Report did not specifically address these competing factors and essentially ignored the likelihood of much more rapid melting of Greenland and other land - based ice sheets.
We contended here before that this is a bit of a leap, since there are other constraints on climate sensitivity (such as the last ice age) and other sources of uncertainty (solar, ozone, land use, etc.).
Charney sensitivity refers to the climate sensitivity when fast - reacting feedbacks (Planck response is a given — also, water vapor, clouds,... I think sea ice, seasonal snow) occur but with other things (land - based ice sheets,... vegetation -LRB-?)-RRB-
Global average temperature is lower during glacial periods for two primary reasons: 1) there was only about 190 ppm CO2 in the atmosphere, and other major greenhouse gases (CH4 and N2O) were also lower 2) the earth surface was more reflective, due to the presence of lots of ice and snow on land, and lots more sea ice than today (that is, the albedo was higher).
I also believe that soot and all the other aerosols that combine and rain out has contributed to significant albedo changes and is food for localized warming from biochemical activity in the boreal north that has significantly contributed to the melting of land and sea ice.
Globally, the Ozzies have pointed out that the oceans have been busy absorbing almost all of the heat energy (90 %) The atmosphere and the land, including ice, store the other 10 %.
On decadal and longer time scales, global mean sea level change results from two major processes, mostly related to recent climate change, that alter the volume of water in the global ocean: i) thermal expansion (Section 5.5.3), and ii) the exchange of water between oceans and other reservoirs (glaciers and ice caps, ice sheets, other land water reservoirs - including through anthropogenic change in land hydrology, and the atmosphere; Section 5.5.5).
The research challenges the conclusions of other studies, including the Intergovernmental Panel on Climate Change's (IPCC) 2013 report, which says that Antarctica is overall losing land ice
The sudden onset and ending of the Younger Dryas has been studied in particular detail in the ice core and sediment records on land and in the sea (e.g., Bjoerck et al., 1996), and it might be representative of other Heinrich events.
Six types of instruments aboard Aqua are to scan through the atmosphere down to the surface, gathering the most detailed data ever on water vapor in clouds, ice crystals in the air, evaporation, water in the oceans, icebergs and other sea ice, as well as glaciers and snow pack on land.
The other rebuttal deals with both land and sea - based ice.
The 2009 State of the Climate Report of the US National Oceanic and Atmospheric Administration (NOAA) tells us that climate change is real because of rising surface air temperatures since 1880 over land and the ocean, ocean acidification, sea level rise, glaciers melting, rising specific humidity, ocean heat content increasing, sea ice retreating, glaciers diminishing, Northern Hemisphere snow cover decreasing, and so many other lines of evidence.
Over the long - term, melting of the West Antarctic Ice Sheet could yield as much as 10 to 14 feet of global average sea level rise, with local sea level rise varying considerably depending on land elevation trends, ocean currents and other factors.
The other papers also show that sea level rise acceleration post-1990, predominately due to increased land ice melt:
The supposed stable configuration of geography, with relatively predictable climate patterns, coastlines and icepacks in familiar locations, and clear demarcations of territorial control on land are increasingly dubious assumptions as weather patterns change, sea levels rise and ice packs disintegrate while technological innovations, communications and global markets cause rapid fluctuations in the price in food and other essentials across boundaries.
Responsible skepticism would not assert that an error about the rate of Himalayan ice melt or the the amount of land in the Netherlands below sea - level was proof that an enormous body of scientific literature on other climate change issues was fraudulent.
Greenland's ice has been melting faster than many scientists expected just a decade ago, spurred by warming sea and land temperatures, changing weather patterns, and other factors.
Over Greenland and other ice - covered land areas the snow product is not available (green areas).
Other than the melting of land ice (which would have to involve warming of course) I can not think of another mechanism, can you?
Other areas of reduced sea ice cover are the Southern Ocean north of Dronning Maud Land, and the area west of the Ross Sea and north of Wilkes Land.
Yes, I have been to nsidc.org a fair amount, particularly this page to try to understand each Northern Hemisphere summer what is going on with greenland ice melt: http://nsidc.org/greenland-today/ While I do like that page, I must say I have not been able to find what I am looking for there, as far as clear non-scientist-oriented data that shows land ice changes over the years, whether for the Antarctic, Greenland or other places.
«By contrast, the eastern Antarctic and Antarctic plateau have cooled, primarily in summer, with warming over the Antarctic Peninsula [C3 Ed: approximately 4 % of Antarctica land mass]... Moreover, sea - ice extent around Antarctica has modestly increased... In other words, the authors find that most of the Antarctic continent has cooled, rather than just the Southern Ocean...»
The climate models that scientists use to understand and project climate change are improving constantly, with better representations of the oceans, ice, land surfaces and other factors in the atmosphere.
On the other hand they melt fast when a rising ocean hits their boundary and turns landlocked ice directly into dark ocean surface with no intermediate state of ice - free land surface.
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