Warm ocean currents make surrounding areas warmer and rainy.
Not exact matches
Map of
current land and ice separating the Weddell and Ross seas, courtesy of Wikimedia Commons / Wutsje / CIA Octopuses have
made themselves at home in most of the world's
oceans — from the
warmest of tropical seas to the deep, dark reaches around hydrothermal vents.
The
currents flowing across the sill bring
warm Atlantic water into the polar sea, and although the net gain each year is tiny, over thousands of years it is enough to
make the Arctic
Ocean very much
warmer.
Water from the melting ice
makes the
oceans rise, only a fraction of an inch a year but, in the fullness of time, enough to let the
currents increase their flow over the northern sill, bringing ever more
warm water into the gelid Arctic.
Now, this will
make many readers mad, but does a
warming world with
ocean currents, acidification changes have anything to do with this?
Previous large natural oscillations are important to examine: however, 1) our data isn't as good with regards to external forcings or to historical temperatures,
making attribution more difficult, 2) to the extent that we have solar and volcanic data, and paleoclimate temperature records, they are indeed fairly consistent with each other within their respective uncertainties, and 3) most mechanisms of internal variability would have different fingerprints: eg, shifting of warmth from the
oceans to the atmosphere (but we see
warming in both), or simultaneous
warming of the troposphere and stratosphere, or shifts in global temperature associated with major
ocean current shifts which for the most part haven't been seen.
Rising surface temperatures in the last three decades of the 20th century were roughly half caused by man -
made global
warming and half by the
ocean currents keeping more heat near the surface, it finds.
For example, reductions in seasonal sea ice cover and higher surface temperatures may open up new habitat in polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of cold bottom - water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering Sea and Chukchi Sea off northwestern Alaska.129, 130 In addition,
warming may cause reductions in the abundance of some species, such as pollock, in their
current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If
ocean warming continues, it is unlikely that
current fishing pressure on pollock can be sustained.133 Higher temperatures are also likely to increase the frequency of early Chinook salmon migrations,
making management of the fishery by multiple user groups more challenging.134
The paper being discussed here
makes the claim that the
current hiatus in
warming is due to the heat going into the Atlantic
ocean as the Atlantic
ocean is currently in the 30 year cooling phase of it's ~ 60 year
warming / cooling cycle.
The only way we could get runaway
warming would be to
make the
ocean currents as close to frictionless as we could.
Cool
ocean currents make surrounding areas cooler and drier Warmer and Rainy Warm Ocean Current Cooler and Drier Cool Ocean Cu
ocean currents make surrounding areas cooler and drier
Warmer and Rainy
Warm Ocean Current Cooler and Drier Cool Ocean Cu
Ocean Current Cooler and Drier Cool
Ocean Cu
Ocean Current
Perversely, an abnormally
warm current to the Arctic would cause
warming of the atmosphere while reducing heat content in the
ocean,
making it appear as if the earth is
warming when in fact it is cooling.