Not exact matches
This year, the Atlantic was warmer than
average — Klotzbach says August through October will likely rank third or fourth
in terms
of highest tropical Atlantic
Ocean temperatures.
The properties
of the climate system include not just familiar concepts
of averages of temperature, precipitation, and so on but also the state
of the
ocean and the cryosphere (sea ice, the great ice sheets
in Greenland and Antarctica, glaciers, snow, frozen ground, and ice on lakes and rivers).
The main drivers
of El Niño conditions,
ocean temperatures in the central and eastern Pacific, were as high as 3 °C above the
average, making this event one
of the three most intense El Niños on record.
But climate models predict reductions
in dissolved oxygen
in all
oceans as
average global air and sea
temperatures rise, and this may be the main driver
of what is happening there, she says.
As
of March 2013, surface waters
of the tropical north Atlantic
Ocean remained warmer than
average, while Pacific
Ocean temperatures declined from a peak
in late fall.
But within these long periods there have been abrupt climate changes, sometimes happening
in the space
of just a few decades, with variations
of up to 10ºC
in the
average temperature in the polar regions caused by changes
in the Atlantic
ocean circulation.
However, certain areas
in the
oceans could be unusually warm and skew the overall long - term
average temperature results
of some
of those prior studies, Shuman says.
Their findings, based on output from four global climate models
of varying
ocean and atmospheric resolution, indicate that
ocean temperature in the U.S. Northeast Shelf is projected to warm twice as fast as previously projected and almost three times faster than the global
average.
According to NOAA, the global
average ocean temperature for the first half
of the year is 1.42 °F (0.79 °C) above the 20th century
average, the largest such departure
in 137 years
of records.
The man - made part
of the disaster, caused by burning fossil fuels, has increased
ocean temperature an
average of 1.33 degrees Fahrenheit since the start
of the Industrial Revolution, according to a study
in Science.
Average global land and
ocean temperatures have climbed at a rate
of 0.2 °C per decade since 1976, according to data compiled by the National Climatic Data Center (NCDC)
in Asheville, North Carolina, and the World Meteorological Organization (WMO)
in Geneva, Switzerland.
So the report notes that the current «pause»
in new global
average temperature records since 1998 — a year that saw the second strongest El Nino on record and shattered warming records — does not reflect the long - term trend and may be explained by the
oceans absorbing the majority
of the extra heat trapped by greenhouse gases as well as the cooling contributions
of volcanic eruptions.
The CPC officially considers it an event when the sea surface
temperatures in a key region
of the
ocean reach at least 0.5 °C, or about 1 °F, warmer than
average.
El Niño is characterized by a large area
of warmer - than -
average ocean surface
temperatures in the central and eastern Pacific.
Any reforms to come from the process, starting next week, would affect about 62 percent
of New York state's population, the proportion estimated to reside now
in areas that could be hard hit as rising land and
ocean temperatures raise
average sea levels around the globe.
The researchers found that phytoplankton
in polar and temperate regions grow best at
temperatures higher than the
average annual
temperatures of the
oceans in which they live.
The June 2013 globally -
averaged temperature across
ocean surfaces was the 10th highest
in the 134 - year period
of record, at 0.48 °C (0.86 °F) above the 20th century
average.
With higher levels
of carbon dioxide and higher
average temperatures, the
oceans» surface waters warm and sea ice disappears, and the marine world will see increased stratification, intense nutrient trapping
in the deep Southern
Ocean (also known as the Antarctic
Ocean) and nutrition starvation
in the other
oceans.
Time series
of temperature anomaly for all waters warmer than 14 °C show large reductions
in interannual to inter-decadal variability and a more spatially uniform upper
ocean warming trend (0.12 Wm − 2 on
average) than previous results.
«The
average ocean temperature is much warmer than Siberia, initially suggesting that the formation
of subsea pingos could not be recent, as anticipated for pingos
in cold Siberian environments.
Global mean
temperatures averaged over land and
ocean surfaces, from three different estimates, each
of which has been independently adjusted for various homogeneity issues, are consistent within uncertainty estimates over the period 1901 to 2005 and show similar rates
of increase
in recent decades.
The ratio
of these gases
in the atmosphere therefore allows for the calculation
of average global
ocean temperature.
These rising atmospheric greenhouse gas concentrations have led to an increase
in global
average temperatures of ~ 0.2 °C decade — 1, much
of which has been absorbed by the
oceans, whilst the oceanic uptake
of atmospheric CO2 has led to major changes
in surface
ocean pH (Levitus et al., 2000, 2005; Feely et al., 2008; Hoegh - Guldberg and Bruno, 2010; Mora et al., 2013; Roemmich et al., 2015).
The warmth was due to the near - record strong El Niño that developed during the Northern Hemisphere spring
in the eastern and central equatorial Pacific
Ocean and to large regions of record warm and much warmer - than - average sea surface temperatures in parts of every major ocean b
Ocean and to large regions
of record warm and much warmer - than -
average sea surface
temperatures in parts
of every major
ocean b
ocean basin.
(1) The warm sea surface
temperatures are not just some short - term anomaly but are part
of a long - term observed warming trend,
in which
ocean temperatures off the US east coast are warming faster than global
average temperatures.
The December 2015 globally -
averaged temperature across land and
ocean surfaces was 1.11 °C (2.00 °F) above the 20th century
average of 12.2 °C (54.0 °F), the highest for any month since records began
in 1880, surpassing the previous all - time record set two months ago
in October by 0.12 °C (0.21 °F).
It was cooler than
average in eastern Russia, regions of central and northern Africa, and part of central South America, according to the December Land & Ocean Temperatures Departure from Average and Percentiles maps
average in eastern Russia, regions
of central and northern Africa, and part
of central South America, according to the December Land &
Ocean Temperatures Departure from
Average and Percentiles maps
Average and Percentiles maps above.
The June globally
averaged sea surface
temperature was 1.39 °F above the 20th century monthly
average of 61.5 °F — the highest global
ocean temperature for June
in the 1880 — 2016 record, surpassing the previous record set
in 2015 by 0.05 °F.
The May globally
averaged sea surface
temperature was 1.37 °F above the 20th century monthly
average of 61.3 °F — the highest global
ocean temperature for May
in the 1880 — 2016 record, surpassing the previous record set
in 2015 by 0.09 °F.
Linear trend (1955 — 2003)
of zonally
averaged temperature in the upper 1,500 m
of the water column
of the Atlantic, Pacific, Indian and World
Oceans.
The April globally
averaged sea surface
temperature was 1.44 °F above the 20th century monthly
average of 60.9 °F — the highest global
ocean temperature for April
in the 1880 — 2016 record, surpassing the previous record set
in 2015 by 0.25 °F and besting 1998, the last time a similar strength El Niño occurred, by 0.43 °F.
The July globally
averaged sea surface
temperature was 1.42 °F above the 20th century monthly
average of 61.5 °F — the highest global
ocean temperature for July
in the 1880 — 2016 record, surpassing the previous record set
in 2015 by 0.07 °F.
The Fourth Assessment Report finds that «Warming
of the climate system is unequivocal, as is now evident from observations
of increases
in global
average air and
ocean temperatures, widespread melting
of snow and ice, and rising mean sea level.
The September globally
averaged sea surface
temperature was 1.33 °F above the 20th century monthly
average of 61.1 °F, tying with 2014 as the second highest global
ocean temperature for September
in the 1880 — 2016 record, behind 2015 by 0.16 °F.
Rising CO2 levels have been linked to the globe's
average temperature rise as well as a host
of other changes to the climate system including sea level rise, shifts
in precipitation,
ocean acidification, and an increase
in extreme heat.
Cooling sea - surface
temperatures over the tropical Pacific
Ocean — part
of a natural warm and cold cycle — may explain why global
average temperatures have stabilized
in recent years, even as greenhouse gas emissions have been warming the planet.
Generally above -
average March
temperatures were seen
in the mid-latitudes and tropics both north and south
of the equator, with the exceptions
of eastern Canada, the North Atlantic
Ocean, western Europe, northwest Africa, and central South America.
La Niña is the positive phase
of the El Niño Southern Oscillation and is associated with cooler than
average sea surface
temperatures in the central and eastern tropical Pacific
Ocean.
The
average ocean temperature hovers around 73 degrees
in August, making it the warmest
ocean water off the coast
of California.
For his site - specific project East Meets West, Finch traveled to the Atlantic and Pacific coasts, where he used a colorimeter — a device that measures the
average color and
temperature of light that exists naturally
in a specific place and time — to calculate the color
of the light on the
oceans.
[1] CO2 absorbs IR, is the main GHG, human emissions are increasing its concentration
in the atmosphere, raising
temperatures globally; the second GHG, water vapor, exists
in equilibrium with water / ice, would precipitate out if not for the CO2, so acts as a feedback; since the
oceans cover so much
of the planet, water is a large positive feedback; melting snow and ice as the atmosphere warms decreases albedo, another positive feedback, biased toward the poles, which gives larger polar warming than the global
average; decreasing the
temperature gradient from the equator to the poles is reducing the driving forces for the jetstream; the jetstream's meanders are increasing
in amplitude and slowing, just like the lower Missippi River where its driving gradient decreases; the larger slower meanders increase the amplitude and duration
of blocking highs, increasing drought and extreme
temperatures — and 30,000 + Europeans and 5,000 plus Russians die, and the US corn crop, Russian wheat crop, and Aussie wildland fire protection fails — or extreme rainfall floods the US, France, Pakistan, Thailand (driving up prices for disk drives — hows that for unexpected adverse impacts from AGW?)
With the current GHG content
in the atmosphere, more solar energy arrives than leaves via radiation -LRB-.85 + / -.15 Watt / m ^ 2), which raises the heat content
of the terrestrial system, i.e., the
average temperature over the whole earth +
oceans + atmosphere.
The standard assumption has been that, while heat is transferred rapidly into a relatively thin, well - mixed surface layer
of the
ocean (
averaging about 70 m
in depth), the transfer into the deeper waters is so slow that the atmospheric
temperature reaches effective equilibrium with the mixed layer
in a decade or so.
I also used my implementation to break up a quick land response from a slow
ocean response to see if the change
in sign
of the derived
temperature derivative coming at a place where it is not intersecting the instantaneous
temperature might be explained by the derived
temperature being an
average.
Given all the independent lines
of evidence pointing to
average surface warming over the last few decades (satellite measurements,
ocean temperatures, sea - level rise, retreating glaciers, phenological changes, shifts
in the ranges
of temperature - sensitive species), it is highly implausible that it would lead to more than very minor refinements to the current overall picture.
As the distribution
of land and
ocean areas
in the two hemispheres is markedly different the redistribution
of heat via MOC leaves open the possibility
of the world getting hotter
in the first sense whilst the
averaged temperatures only rise a little or stagnate.
It stands to reason that the
oceans haven't been that warm
in a while but since the
average temperature of the whole mass
of water is so dependent on circulation (it's only the surface
temperature that's constrained by its interactions with the atmosphere and space), I suppose a plausible history
of that particular value would be very hard to reconstruct.
Anthropogenic climate change will mean an increased
average temperature for the
oceans and possible changes
in current systems that could locally amplify or reduce warming and can alter nutrient cycling resulting
in changes
in the amount
of nutrients available for the growth
of phytoplankton, the plant plankton that are the base
of the food chain.
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??
Warming
of the climate system is unequivocal, as is now evident from observations
of increases
in global
average air and
ocean temperatures, widespread melting
of snow and ice, and rising global
average sea level.