The crust encompasses the brittle and shifting continental plates; it becomes scarred with mountains when the plates grind together or with deep
ocean basins when the plates pull apart.
Not exact matches
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.»
For much of the global
ocean the coarser resolution is okay, but
when you are studying a unique location like the Gulf of Maine, with its complex bathymetry of deep
basins, channels, and shallow banks combined with its location near the intersection of two major
ocean current systems, the output from the coarser models can be misleading.»
When I first enter the Surfline homepage, I click on the global swell map to get an idea of what each
ocean basin is doing.
When Santa Ana conditions prevail, with winds in the lower two to three kilometers (1.25 - 1.8 miles) of the atmosphere from the north through east, the air over the coastal
basin is extremely dry, and this dry air extends out over offshore waters of the Pacific
Ocean.
SSTs are a minor portion of
ocean heat content (especially
when we're talking about just a portion of one
basin.)
During epochs
when El Niño events dominate, the SST anomalies of the North Atlantic rise more than the SST anomalies of the other
ocean basins, and
when La Niña events dominate, the North Atlantic SST anomalies drop more than the SST anomalies for the rest of the globe.
The recent papers looking at
ocean ingress into the
basin is also a worry
when we look at the SST's of those waters in Fram and Bering.
I have illustrated and document that there are multiyear aftereffects of ENSO events that cause the positive trends in SST and TLT anomalies outside of the tropical Pacific, and I have shown that the rise in global OHC,
when broken down into logical
ocean basin subsets, is dominated by natural variables.
We found that the two quantities that correlate significantly and consistently in all
ocean basins and seasons are the Hadley cell extent and the high cloud field:
when the Hadley cell edge moves poleward, the high cloud field also shifts towards the poles, and vice versa.
How could the Pacific SST cool
when the heat sink was located in other
ocean basins?
When tectonic plates slide, sink and shift the Earth's continents to form large landmasses, or supercontinents,
ocean basins open and close in tandem.
When a
basin is resonant, energy from the gravitational attraction of the moon aligns with the length of the
ocean basin, causing an amplification of tidal energy.
«Third, in a period
when ocean basins were similar to modern, ice age climate sensitivity to pCO2 changes is underestimated by climate models even
when long term changes in solar forcing and ice sheet size and distribution are taken into account, implying that internal positive feedbacks are stronger than previously thought.»
They used an algorithm to count the number of tropical cyclones that formed in each
ocean basin in the world of 2080 - 2099,
when the assumed SSTs were 2.5 C higher than today's (IPCC A1B scenario).