«The Afar region provides a unique study area for continental breakup and formation of
new ocean basins.»
The repeated cycles of plate tectonics that have led to collision and assembly of large supercontinents and their breakup and formation of
new ocean basins have produced continents that are collages of bits and pieces of other continents.
Rifts are the initial stage of a continental break - up and, if successful, can lead to the formation of
a new ocean basin.
Eventually,
a new ocean basin forms.
Not exact matches
One of the subtle changes visible in the
new data - set is how the Amazon's greenness corresponds to one of the long - known causes of rainfall or drought to the Amazon
basin: changes in sea surface temperatures in the eastern Pacific
Ocean, called the El Nino Southern Oscillation.
One important algae quantified by this
new technique are the coccolithophores,
ocean plants that surround themselves with reflective chalk plates that, en masse, can cause entire
ocean basins to reflect more light when they «bloom.»
«The hypothesis that the floor of the
oceans has been spreading seeks to explain some characteristics of
ocean basins and the continents by supposing that material welling up from the interior of the earth forms mid-
ocean ridges and then, as
new material rises, moves outward, away from the ridges.
«We need to do more studies to be able to determine if this
new species, which we are yet to name, only lives in the shallow waters of the western Mediterranean or if it is also found in other deep water
basins in the eastern Mediterranean or Atlantic
Ocean, for example,» highlights Conxita Àvila.
Monash University geoscientist Associate Professor Wouter Schellart, and his colleague Professor Wim Spakman from Utrecht University, have discovered how the floor of an entire
ocean basin that was destroyed 70 to 50 million years ago off the North coast of
New Guinea is currently located at 800 - 1200 km depth below Central and South - eastern Australia.
Their study demonstrates that since 1982, broad stretches of these
ocean basins have warmed and become significantly more hospitable to these algae and that
new «blooms» of these algae have become common in these same regions.
The
new find confirms that the ancient lavas formed at midocean ridges and found throughout deep
ocean basins are by volume the largest ecosystem on Earth, scientists say.
Using statistical analysis, the
new study shows that even in
ocean basins where reduced wind shear plays a role, warming sea - surface temperature is the dominant driver.
SLR satellite data includes things such as the «GIA Adjustment» — which is the amount of SLR that there would have been if the
ocean basin hadn't increased in volume and in the case of this
new study, how much higher the sea surface would have been if it had not been suppressed by the Mount Pinatubo volcanic eruption, another correction for ENSO / PDO «computed via a joint cyclostationary empirical orthogonal function (CSEOF) analysis of altimeter GMSL, GRACE land water storage, and Argo - based thermosteric sea level from 2005 to present», as well as other additions and adjustments — NONE OF WHICH can actually be found manifested in any change to the physical Sea Surface Height.»
In fact, I have already attempted that and my
New Climate Model not only incorporates that «stadium» wave» as it works through the
ocean basins but also places it within an overall climate change description.
Each beach was located across the Pacific
Ocean basin, throughout the mainland U.S., Canada, Japan, Australia,
New Zealand, and Hawaii.
In the
new study, scientists simulated the movement of Earth's tectonic plates and changes in the resonance of
ocean basins over millions of years.
These experiments provide
new insight into mechanisms of past climate changes on Earth, which have been driven in part by tectonic changes in
ocean basins and consequent changes in
ocean circulation and heat transport.
The
new finding of the importance of multiple
ocean surface temperature changes to the multi-decadal global warming accelerations and slowdowns is supported by a set of computer modeling experiments, in which observed sea surface temperature changes are specified in individual
ocean basins, separately.