Ocean states shift abruptly at these times and are punctuated by extreme El Niño Southern Oscillation events.
Not exact matches
So climatologist James Elsner of Florida
State University in Tallahassee and his colleagues looked for ties between hurricane tracks and the North Atlantic Oscillation (NAO), a seesaw
shift in atmospheric pressures over the
ocean (Science, 12 February 1999, p. 948).
Changing temperatures and
ocean acidification, together with rising sea level and
shifts in
ocean productivity, will keep marine ecosystems in a
state of continuous change for 100,000 years.
The rapid northerly
shifts in spawning may offer a preview of future conditions if
ocean warming continues, according to the new study published in Global Change Biology by scientists from the Pacific
States Marine Fisheries Commission, Oregon
State University and NOAA Fisheries» Northwest Fisheries Science Center.
This abstract print interprets the constantly
shifting states of the
ocean and sky with layers of blue hues and textures.
The workshop summarized the
state of understanding, key uncertainties and next research steps on the
shifting chemistry of the
oceans and the impacts on species and ecosystems, with a focus on ecosystems of particular interest to humans.
One way or the other, it's clear that, by the end of the 1990s, the veneer of ice on the Arctic
Ocean had
shifted to a far more tenuous
state, with ever less thick, years - old ice like the floes I camped on when I went with the team setting up the annual North Pole Environmental Observatory.
More recent work is identifying climate
shifts working through the El Niño - Southern Oscillation (ENSO), Atlantic Multidecadal Oscillation (AMO), Pacific Decadal Oscillation (PDO), North Atlantic Oscillation (NAO), Southern and Northern Annular Modes (SAM and NAM), Artic Oscillation (AO), Indian
Ocean Dipole (IOD), North Pacific Oscillation (NPO) and other measures of ocean and atmospheric st
Ocean Dipole (IOD), North Pacific Oscillation (NPO) and other measures of
ocean and atmospheric st
ocean and atmospheric
states.
These climate
shifts are linked to sychronous changes in
ocean and atmospheric indices and to changes in the Pacific
state.
The Pacific
Ocean shifted again to a somewhat cooler
state after 1998.
It is seen in regime changes in cloud, ice,
ocean and atmospheric circulation, hydrology and biology that are evident in climate records and that are best described as
shifts in
state space on the multi-dimensional climate strange attractor at 20 to 30 year intervals.
Climate
shifts are marked by changes in the
state of the Pacific
Ocean and in the trajectory of atmospheric temperature.
Such things as drops of 10 degrees in places in as little as a decade and abrupt
shifts in hydrology and
ocean states.
Sea levels are rising (ask the Mayor of Miami who has spent tax monies to raise road levels), we've had 15 of the hottest years eve measured, more precipitation is coming down in heavy doses (think Houston), we're seeing more floods and drought than ever before (consistent with predictions), the
oceans are measuring warmer, lake ice in North America is thawing sooner (where it happens in northern
states and Canada), most glaciers are shrinking, early spring snowpacks out west have declined since the 1950's, growing seasons are longer throughout the plains, bird wintering ranges have moved north, leaf and bloom dates recorded by Thoreau in Walden have
shifted in that area, insect populations that used to have one egg - larva - adult cycle in the summer now have two, the list goes on and on.
Ocean and atmosphere circulation
shift climate
states abruptly in completely deterministic but apparently random ways in a complex and dynamic system.
I have hypothesised a solar trigger for
state shifts in
ocean and atmospheric circulation.
Would we for instance change the Mg / Ca ratio triggering
shifts to a calcite rather than the modern aragonite
state of the
oceans?
In a recent study, researchers found that when the Atlantic
Ocean swung from one
state to another, it apparently helped trigger a decade - long climate
shift in the late 1960s that sprang from the Atlantic and reached as far as Australia.