suggests that, in a centennial (as opposed to millennial or more) time frame, climate sensitivity is much higher for
land than ocean, and hence should be higher for the Northern Hemisphere than the Southern.
The magnitude of the spike is larger over
land than ocean, and also largest in the Southern Hemisphere.
Forced changes mediate greater
land than ocean temperature fluctuations due to the thermal inertia of the oceans, the moderating effect of evaporation, and probably other factors.
There's less water over
land than ocean so look for more warming over land than water.
Longer records now available show significantly faster rates of warming over
land than ocean in the past two decades (about 0.27 °C vs. 0.13 °C per decade).
In response to increased trace gases, all replicated the qualitative response seen in other coupled ocean - atmosphere models: greater warming over
land than ocean and maximum warming at high northern latitudes in winter.
In general there is more warming over
land than the oceans and more warming at the poles than in the tropics.
Not exact matches
«The footprint of industrial fishing in the
ocean is over four times larger
than the
land area occupied by agriculture.»
In the past of earlier decades every nation or individuals of any nation were happy to deal or trade or buy from Islamic traders marking them as being most honest and truthful... that's how they were known as traders who's their sea trade extended from Indian
ocean to the China Sea... those other
than the
land transportation by Camel Caravans moving between the South and North as well as between the far East and the far West...!!
When Vasco de Gama rounded the Cape of Good Hope, crossed the Indian
Ocean, and
landed in India in 1498, he established the trade route for spices and other goods that the Portuguese controlled for more
than a century.
He also gave the reasons for skipping any interviews, a decision which
landed him with the sizeable fine - although surely it's little more
than a drop in the
ocean for someone like Max.
Longer timescales bring changes in vegetation that also affect heat absorption, and the possibility that
land and
oceans begin to release CO2 rather
than absorb it.
Tiny plastic particles also present a threat to creatures on
land and may have damaging effects similar or even more problematic
than in our
oceans.
«The range of viable sizes for mammals in the
ocean is actually smaller
than the range of viable sizes on
land,» Payne said.
The study found that more
than 4.8 million metric tons of plastic waste enters the
oceans from
land each year, and that figure may be as high as 12.7 million metric tons.
Previous studies have documented the impact of plastic debris on more
than 660 marine species — from the smallest of zooplankton to the largest whales, including fish destined for the seafood market — but none have quantified the worldwide amount entering the
ocean from
land.
They include higher sea surface temperatures over the Indian
Ocean, which can lead to greater rainfall over the sea rather
than on
land.
As a result of such breakups, more
than 150 cubic kilometers of glacial ice has slid off
land into the
ocean.
Scientists think that massive volcanic eruptions killed off more
than 90 % of
ocean species and 75 % of
land species almost 252 million years ago.
Ocean life does not exist separately from
land life any more
than the Olympic Mountains are separate from the undersea volcanoes that spawned them.
Since the emissions today are three times higher
than they were in the 1960s, this increased uptake by
land and
ocean is not only surprising; it's good news.
If an impactor
landed in the deep
ocean, it wouldn't create much shocked quartz either, because the
ocean floor has less quartz in it
than continental crust.
The collection of larger
than usual amounts of Arctic winter weather data in 2015 was due to two reasons: the Norwegian research vessel Lance was in the Arctic
Ocean observing and collecting upper atmosphere meteorological data, and the frequency of observation and data collection was increased at some of the
land - based observation stations around the Arctic.
A glaciologist rather
than a biologist, he wanted to investigate a question critical to climate change: Do subglacial rivers and lakes lubricate the movement of ice over
land — and might they somehow accelerate a glacier's flow into the
ocean, triggering rapid sea level rise?
-- ice a few feet or yards thick, floating over a deep
ocean; ice more
than a mile thick, over
land; or a mainly rocky, mountainous landscape.
Only 30 percent of respondents answered the sea - level question correctly; Greenland and Antarctic
land ice have much greater potential to raise sea level
than Arctic sea ice, which is already floating on the
ocean.
The advantage of having a lower generator and consequently a lower center of gravity helps lower installation costs on floating platforms in the
ocean, where wind speed is typically higher
than on
land, observed Veers.
Land - based impacts were, on average, an order of magnitude more dangerous
than asteroids that
landed in
oceans.
Water changes temperature more slowly
than the air or
land, which means the global
ocean heat is likely to persist for some time.
These variations originate primarily from fluctuations in carbon uptake by
land ecosystems driven by the natural variability of the climate system, rather
than by
oceans or from changes in the levels of human - made carbon emissions.
Typical
ocean crust is just 4 miles (6 km) thick, roughly five times thinner
than the crust that lies below
land - based volcanoes.
Because the vast plateau at such altitudes absorbs a huge amount of solar radiation, the atmospheric layer above it in summer is much warmer
than air at similar elevations over lower
land or the
oceans.
The effect was easier to see over water
than land because, in general, the atmosphere above the
oceans is relatively low in aerosols — tiny liquid or solid particles that float in the air.
What scientists discovered in 2014 is that since the turn of the century,
oceans have been absorbing more of global warming's heat and energy
than would normally be expected, helping to slow rates of warming on
land.
That is because it is one of the few active rifts on
land rather
than in the depths of the old
oceans.
Studies of past climate changes suggest the
land and
oceans start releasing more CO2
than they absorb as the planet warms.
June — August 2014, at 0.71 °C (1.28 °F) higher
than the 20th century average, was the warmest such period across global
land and
ocean surfaces since record keeping began in 1880, edging out the previous record set in 1998.
With records dating back to 1880, the global temperature across the world's
land and
ocean surfaces for August 2014 was 0.75 °C (1.35 °F) higher
than the 20th century average of 15.6 °C (60.1 °F).
«We now know that the changes in the
ocean are happening between 1.5 and 5 times faster
than those on
land,» he added in the report.
This hotter mantle would have made the crust beneath the
oceans hotter and thicker
than it is today, buoying it up relative to the continents, and the associated shallower
ocean basins would have held less water, leading to the flooding of much of what is now
land.
However, for the globe as a whole, surface air temperatures over
land have risen at about double the
ocean rate after 1979 (more
than 0.27 °C per decade vs. 0.13 °C per decade), with the greatest warming during winter (December to February) and spring (March to May) in the Northern Hemisphere.
After over three billion years of evolution in the
oceans, multi-cellular life — beginning with green algae, fungi, and plants (liverworts, mosses, ferns, then vascular and flowering plants)-- began adapting to
land habitats by creating a new «hypersea,» and adding anomalous shades of green to Earth's coloration more
than 472 million years ago (Matt Walker, BBC News, October 12, 2010; and Qiu et al, 1998 — more on the evolution of photosynthetic life and plants on Earth).
This Tuesday, for example, SpaceX will run a test launch of its Falcon 9 rocket and will attempt to
land it on a floating platform in the Atlantic
Ocean, rather
than allowing it to splash down into the water as it has on previous tests.
The observed fact that temperatures increases slower over the
oceans than over
land demonstrates that the large heat capacity of the
ocean tries to hold back the warming of the air over the
ocean and produces a delay at the surface but nevertheless the atmosphere responds quit rapidly to increasing greenhouse gases.
It has been known since far before industrial times that
land heats faster
than the
oceans.
The observed patterns of warming, including greater warming over
land than over the
ocean, and their changes over time, are only simulated by models that include anthropogenic forcing.
Warming, particularly since the 1970s, has generally been greater over
land than over the
oceans.
Paul S also noted that much of the NH / SH ratio comes from the greater
land /
ocean warming ratio in the NH
than is generally modelled, which is another mystery.
Furthermore, basic physical understanding supports the modeled value of E being substantially greater
than 1, as deep
oceans clearly take longer to respond
than the
land surface, so the Northern Hemisphere, with most of the world's
land, will respond more rapidly
than the Southern Hemisphere with more
ocean.
The former is likely to overestimate the true global SAT trend (since the
oceans do not warm as fast as the
land), while the latter may underestimate the true trend, since the SAT over the
ocean is predicted to rise at a slightly higher rate
than the SST.