Not exact matches
We don't know exactly how much plastic is floating in our
oceans because of the huge
mass of plastic produced in the earth on a yearly
basis.
Visitors can enter models of the explorers»
base camps and view a computer map of Antarctica outlining the
ocean currents around the continent and the land
masses and mountains that lie hidden beneath the ice.
By linking worldwide data on solid waste, population density, and economic status, we estimated the
mass of land -
based plastic waste entering the
ocean.
The extent of the ice in the Arctic has always been very uncertain but, through this work, we show how the sea ice in the Arctic
Ocean developed before all the land -
based ice
masses in the Northern Hemisphere were established,» Jochen Knies explains.
The only time period that remotely resembles the
ocean changes happening today,
based on geologic records, was 56 million years ago when carbon mysteriously doubled in the atmosphere, global temperatures rose by approximately six degrees and
ocean pH dropped sharply, driving up
ocean acidity and causing a
mass extinction among single - celled
ocean organisms.
However, if the remaining ice shelf collapses or starts losing
mass more rapidly, it could effectively unplug the glaciers next to the shelf, sending land -
based ice into Southern
Ocean, and contributing to sea level rise.
Furthermore, by knowing the
mass of a planet from radial velocity measurements and the radius of a planet
based on how much starlight it blocked, it is a simple calculation to determine a planet's density, which can tell astronomers whether that planet is rocky or gaseous in nature, or whether it has a small core and a thick atmosphere, or whether it has a large core covered in deep
oceans.
Omega - joint —
based on chicken and flaxseed providing
masses of absorbable Omega - 3's, as is the Omega - derm — from Vetologica, makes a big difference to some of these cats and is not depleting our
oceans of fish.
Consistent with how I was reading things, pleasantly — barring some cautious hedging I'd made,
based on the possibility that salinity could reflect
mass changes, either when fresh water was added to the
ocean via glacial melt or impoundment decreases (
ocean mass increase) or via increased evaporation rates (
ocean mass decrease).
This estimate is
based on the carbon
mass in the atmosphere and up take rates for the
oceans and terrestrial biosphere.
Sea level change
based on satellite altimetry is measured with respect to the Earth's centre of
mass, and thus is not distorted by land motions, except for a small component due to large - scale deformation of
ocean basins from GIA.
That may be true on a total
mass basis, however, the comparison of the water
mass versus the
mass of only the top crust, that part that is visible for example, down a few kilometers, say to the depth of the deepest part of the
ocean — water would be a significantly higher proportion of the
mass than you have stipulated.
We know from satellite measurements that the Greenland and West Antarctic ice sheets (GIS and WAIS respectively) are losing
mass in response to global warming, and that, in the case of the partly sea -
based West Antarctica ice - sheet, basal melting of the ice by warmer
ocean - water is likely to be a key mechanism.
We quantify sea - level commitment in the baseline case by building on Levermann et al. (10), who used physical simulations to model the SLR within a 2,000 - y envelope as the sum of the contributions of (i)
ocean thermal expansion,
based on six coupled climate models; (ii) mountain glacier and ice cap melting,
based on surface
mass balance and simplified ice dynamic models; (iii) Greenland ice sheet decay,
based on a coupled regional climate model and ice sheet dynamic model; and (iv) Antarctic ice sheet decay,
based on a continental - scale model parameterizing grounding line ice flux in relation to temperature.
I would suggest that a new proxy for heat being stored (or lost) from the Earth climate system be developed
based on Total System Enthalpy, using a combination of moist enthalpy in the troposphere (after Pielke Sr.),
ocean heat content, and total ice
mass on the planet.
To conduct the research, a team of scientists led by John Fasullo of the US National Center for Atmospheric Research in Boulder, Colorado, combined data from three sources: NASA's GRACE satellites, which make detailed measurements of Earth's gravitational field, enabling scientists to monitor changes in the
mass of continents; the Argo global array of 3,000 free - drifting floats, which measure the temperature and salinity of the upper layers of the
oceans; and satellite -
based altimeters that are continuously calibrated against a network of tide gauges.
The extent of the ice in the Arctic has always been very uncertain but, through this work, we show how the sea ice in the Arctic
Ocean developed before all the land -
based ice
masses in the Northern Hemisphere were established,» Jochen Knies explains.
I said: - 3oC warmer
oceans =
mass reef death - 3oC warmer earth = very large sea level rise - acidic
oceans are threat to marine life You say this is only
based on models.
But we can infer the sign and (rough) magnitude of the present and past (integrated) TOA imbalance from the combined effect on
ocean heat content and the
mass of the land
based cryosphere.
The Introduction to Levitus et al (2005) begins:
Based on the physical properties and
mass of the world
ocean as compared to other components of Earth's climate system, Rossby [1959]...