During times of warmth, the ocean water levels rise as atmospheric moisture increases but at a rate decelerating when
atmospheric temperatures over oceans approach say 33 C.
Not exact matches
The exceptional strengthening of a high - pressure area in Siberia, which brought freezing
temperatures to Finland in late February and early March, may be partly the result of
atmospheric warming
over the Arctic
Ocean.
Another principal investigator for the project, Laura Pan, senior scientist at the National Center for
Atmospheric Research in Boulder, Colo., believes storm clusters
over this area of the Pacific are likely to influence climate in new ways, especially as the warm
ocean temperatures (which feed the storms and chimney) continue to heat up and
atmospheric patterns continue to evolve.
But
ocean temperatures alone don't define an El Niño; CPC forecasters also look for the corresponding shifts in
atmospheric patterns, namely a weakening of the typical east - to - west trade winds
over the region.
Increased levels of
atmospheric carbon dioxide could also significantly alter
ocean temperatures and chemistry
over the next century, which could lead to increased and more severe mass bleaching and other stressors on coral reefs.
• The methanetrack.org website has shown significant increases in
atmospheric methane concentrations
over Antarctica this austral winter (which I believe are due to increases in methane emissions from the Southern
Ocean seafloor due to increases in the
temperature of bottom water
temperatures), and if this trend continues, then the Southern Hemisphere could be a significant source of additional
atmospheric methane (this century).
However,
atmospheric CO2 content plays an important internal feedback role.Orbital - scale variability in CO2 concentrations
over the last several hundred thousand years covaries (Figure 5.3) with variability in proxy records including reconstructions of global ice volume (Lisiecki and Raymo, 2005), climatic conditions in central Asia (Prokopenko et al., 2006), tropical (Herbert et al., 2010) and Southern
Ocean SST (Pahnke et al., 2003; Lang and Wolff, 2011), Antarctic temperature (Parrenin et al., 2013), deep - ocean temperature (Elder eld et al., 2010), biogeochemical conditions in the Northet al., 2
Ocean SST (Pahnke et al., 2003; Lang and Wolff, 2011), Antarctic
temperature (Parrenin et al., 2013), deep -
ocean temperature (Elder eld et al., 2010), biogeochemical conditions in the Northet al., 2
ocean temperature (Elder eld et al., 2010), biogeochemical conditions in the Northet al., 2008).
Is there a discernible point, maybe in a model, that includes reduced albedo in the summer, that might show an acceleration of melting above the average
temperature increase curve for the region so that
ocean warmth has an increasing role
over atmospheric??
You may now understand why global
temperature, i.e.
ocean heat content, shows such a strong correlation with
atmospheric CO2
over the last 800,000 years — as shown in the ice core records.
1) It seems to me that the key mechanism for any impact must be the changes that increased arctic
ocean temperatures will impose on the
atmospheric circulation feature known as the Polar Cell, and via this on the Ferrel cell which sits
over the mid latitudes.
The first is climate inertia — on very many levels, from fossil lock - in emissions (decades),
ocean -
atmospheric temperature inertia (yet more decades), Earth system
temperature inertia (centuries to millennia) to ecological climate impact inertia (impacts becoming worse
over time under a constant stress)-- all this to illustrate anthropogenic climate change, although already manifesting itself, is still very much an escalating problem for the future.
Comparison of global lower troposphere
temperature anomaly
over the
oceans (blue line) to a model based on the first derivative of
atmospheric CO2 concentration at Mauna Loa (red line).
southern oscillation a large - scale
atmospheric and hydrospheric fluctuation centered in the equatorial Pacific
Ocean; exhibits a nearly annual pressure anomaly, alternatively high over the Indian Ocean and high over the South Pacific; its period is slightly variable, averaging 2.33 years; the variation in pressure is accompanied by variations in wind strengths, ocean currents, sea - surface temperatures, and precipitation in the surrounding
Ocean; exhibits a nearly annual pressure anomaly, alternatively high
over the Indian
Ocean and high over the South Pacific; its period is slightly variable, averaging 2.33 years; the variation in pressure is accompanied by variations in wind strengths, ocean currents, sea - surface temperatures, and precipitation in the surrounding
Ocean and high
over the South Pacific; its period is slightly variable, averaging 2.33 years; the variation in pressure is accompanied by variations in wind strengths,
ocean currents, sea - surface temperatures, and precipitation in the surrounding
ocean currents, sea - surface
temperatures, and precipitation in the surrounding areas
Given the context of this highly anomalous and extremely persistent
atmospheric ridging
over the northeastern Pacific
Ocean, it's very interesting to note that there has also been a region of strongly positive sea surface
temperature anomalies in same the general vicinity for the past 10 - 11 months.
C: increase in
atmospheric CO2 from pre-industrial to present is anthropogenic (D / A) S: best guess for likely climate sensitivity (NUM) s: 2 - sigma range of S (NUM) a:
ocean acidification will be a problem (D / A) L: expected sea level rise by 2100 in cm (all contributions)(NUM) B: climate change will be beneficial (D / A) R: CO2 emissions need to be reduced drastically by 2050 (D / A) T: technical advances will take care of any problems (D / A) r: the 20th century global
temperature record is reliable (D / A) H:
over the last 1000 years global
temperature was hockey stick shaped (D / A) D: data has been intentionally distorted by scientist to support the idea of anthropogenic climate change (D / A) g: the CRU - mails are important for the science (D / A) G: the CRU - mails are important otherwise (D / A)
It is currently suspected, for example, that the recent increase in deep -
ocean heat content is driven by geothermal sources rather than
atmospheric (which would solve the «paradox» that shallow
ocean temperatures,
over the same period, have fallen slightly).
Average air
temperatures over the Arctic
Ocean were much higher than normal for the month, reflecting unusual
atmospheric conditions.
By examining the spatial pattern of both types of climate variation, the scientists found that the anthropogenic global warming signal was relatively spatially uniform
over the tropical
oceans and thus would not have a large effect on the
atmospheric circulation, whereas the PDO shift in the 1990s consisted of warming in the tropical west Pacific and cooling in the subtropical and east tropical Pacific, which would enhance the existing sea surface
temperature difference and thus intensify the circulation.
But matters are greatly complicated by
atmospheric circulation patterns, cyclic changes in
temperatures over the
oceans, and the shapes of land masses.
Also, recent research has tied 20th century
temperature fluctuations in northern California, and much of the Pacific Northwest, to naturally occurring
atmospheric /
ocean circulation patterns over the Pacific O
ocean circulation patterns
over the Pacific
OceanOcean.
It's a mode of natural variation in the tropical eastern Pacific
ocean which is indicated by sea surface
temperature in that region, as well as patterns of
atmospheric pressure, surface winds
over the
ocean, even precipitation
over a much larger region.
In particular, initial stages of
atmospheric model development often take place without coupling to an
ocean model, running instead
over observed sea surface
temperatures (SSTs) and sea ice extent.
The basic point and the one relevant to climate change, is still relevant —
oceans still have an enormous moderating effect on
temperature over time (though if there is a huge increase or decrease in re radiated
atmospheric heat it is going to then affect the
oceans initially).
* Extremely high geopotential heights (a vertically aggregated measure of
atmospheric temperature)
over the northeastern Pacific
Ocean are historically linked to very low precipitation in California.
The recent
atmospheric circulation has driven near normal surface air
temperatures (see Figure 7)
over much of the central Arctic
Ocean (normal compared to a 1981 - 2010 climatology) in the last two months.
In general, the pattern of change in return values for 20 - year extreme
temperature events from an equilibrium simulation for doubled CO2 with a global
atmospheric model coupled to a non-dynamic slab
ocean shows moderate increases
over oceans and larger increases
over land masses (Zwiers and Kharin, 1998; Figure 9.29).
Scientific confidence of the occurrence of climate change include, for example, that
over at least the last 50 years there have been increases in the
atmospheric concentration of CO2; increased nitrogen and soot (black carbon) deposition; changes in the surface heat and moisture fluxes
over land; increases in lower tropospheric and upper
ocean temperatures and
ocean heat content; the elevation of sea level; and a large decrease in summer Arctic sea ice coverage and a modest increase in Antarctic sea ice coverage.
They find that the different moisture availability
over land and
ocean leads to different
atmospheric temperature lapse rates (latent heat release), which in combination with a well - mixed free (above boundary layer) atmosphere can explain the land — sea contrast.
If you have good measurements of upper
ocean and
atmospheric temperatures, then if you had a good decade - long satellite record of the Earth's total radiative energy balance from space — say, if Triana has been launched to in the late 1990s — then you could use conservation of energy to calculate the rate of heat uptake by the deep
ocean over the past ten years.
The SST was largely irrelevant in these scenarios, as the small change in
ocean temperature pales in comparison to the large change in
atmospheric temperature over the land in the central US.
«[S] urface
temperature, averaged
over the land and
ocean, increased only about 1.5 degrees between 1880 to 2012 despite a reputed 36 percent rise in
atmospheric CO ² content.