«Assessing recent warming using instrumentally homogeneous sea surface temperature records» «Tracking ocean heat uptake during the surface warming hiatus» «A review
of global ocean temperature observations: Implications for ocean heat content estimates and climate change» «Unabated planetary warming and its ocean structure since 2006»
Ocean warming: «Assessing recent warming using instrumentally homogeneous sea surface temperature records» «Tracking ocean heat uptake during the surface warming hiatus» «A review
of global ocean temperature observations: Implications for ocean heat content estimates and climate change» «Unabated planetary warming and its ocean structure since 2006»
A review
of global ocean temperature observations: Implications for ocean heat content estimates and climate change
Not exact matches
The Tibetan Plateau in China experiences the strongest monsoon system on Earth, with powerful winds — and accompanying intense rains in the summer months — caused by a complex system
of global air circulation patterns and differences in surface
temperatures between land and
oceans.
Curtis Deutsch, associate professor at the University
of Washington's School
of Oceanography, studies how increasing
global temperatures are altering the levels
of dissolved oxygen in the world's
oceans.
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.
In addition to the Asia heat wave, those events were the record
global heat in 2016 and the growth and persistence
of a large swath
of high
ocean temperatures, nicknamed «the Blob,» in the Bering Sea off the coast
of Alaska.
Antarctica was also more sensitive to
global carbon dioxide levels, Cuffey said, which increased as the
global temperature increased because
of changing
ocean currents that caused upwelling
of carbon - dioxide - rich waters from the depths
of the
ocean.
The resulting outburst
of methane produced effects similar to those predicted by current models
of global climate change: a sudden, extreme rise in
temperatures, combined with acidification
of the
oceans.
The ability
of the
oceans to take up carbon dioxide can not keep up with the rising levels
of greenhouse gases in the atmosphere, which means carbon dioxide and
global temperatures will continue to increase unless humans cut their carbon dioxide emissions.
One
of the biggest lingering issues in the
global warming slowdown is the full impact
of the natural
temperature cycles
of Earth's
oceans.
Indeed, scientists at Scripps recently suggested that 1,800 - year cycles
of ocean tides could drive a natural rise in
global temperatures.
One
of the sturdiest pillars
of the argument against
global warming has crumbled under the weight
of some 10 million newly compiled measurements
of ocean temperature.
As
global temperature rises, most
of the extra heat in the atmosphere — about 90 percent — sinks into the
ocean.
Global warming is also contributing to the rising
ocean temperatures on the whole, but «the warming
of the
ocean alone is not sufficient to explain what we see,» said Eric Rignot, a glacier expert at the University
of California, Irvine, in an emailed comment on the new study.
Land and
Ocean Combined: The combined average temperature over global land and ocean surfaces for August 2014 was the record highest for the month, at 61.45 °F (16.35 °C), or 1.35 °F (0.75 °C) above the 20th century average of 60.1 °F (15.6
Ocean Combined: The combined average
temperature over
global land and
ocean surfaces for August 2014 was the record highest for the month, at 61.45 °F (16.35 °C), or 1.35 °F (0.75 °C) above the 20th century average of 60.1 °F (15.6
ocean surfaces for August 2014 was the record highest for the month, at 61.45 °F (16.35 °C), or 1.35 °F (0.75 °C) above the 20th century average
of 60.1 °F (15.6 °C).
NOAA said the combined
global land and
ocean average surface
temperature for the January - October period was 0.68 °C (1.22 °F) above the 20th century average
of 14.1 °C (57.4 °F).
Ocean Only: The August
global sea surface
temperature was 1.17 °F (0.65 °C) above the 20th century average
of 61.4 °F (16.4 °C), the highest on record for August.
Ocean Only: The June - August
global sea surface
temperature was 1.13 °F (0.63 °C), above the 20th century average
of 61.5 °F (16.4 °C), the highest for June - August on record.
«Many impacts respond directly to changes in
global temperature, regardless
of the sensitivity
of the planet to human emissions
of CO2 and other greenhouse gases,» says geoscientist Katharine Hayhoe
of Texas Tech University in Lubbock, a co-author
of the report, excluding effects such as
ocean acidification and CO2 as a fertilizer for plants.
By next year, the Argo project will have installed 3,000 floating sensors across all the
oceans, offering a daily snapshot
of global patterns
of water
temperature and salinity — crucial for predicting the nature and pace
of climate change.
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.
«Our research indicates that as
global warming continues, parts
of East Antarctica will also be affected by these wind - induced changes in
ocean currents and
temperatures,» Dr Jourdain said.
«When we included projected Antarctic wind shifts in a detailed
global ocean model, we found water up to 4 °C warmer than current
temperatures rose up to meet the base
of the Antarctic ice shelves,» said lead author Dr Paul Spence from the ARC Centre
of Excellence for Climate System Science (ARCCSS).
The area boasts the world's warmest
ocean temperatures and vents massive volumes
of warm gases from the surface high into the atmosphere, which may shape
global climate and air chemistry enough to impact billions
of people worldwide.
The experiment
of the Kiel marine biologists shows how local environmental factors such as eutrophication may amplify the effects
of global factors such as rising
temperatures and
ocean acidification.
«By prescribing the effects
of human - made climate change and observed
global ocean temperatures, our model can reproduce the observed shifts in weather patterns and wildfire occurrences.»
«Atlantic / Pacific
ocean temperature difference fuels US wildfires: New study shows that difference in water
temperature between the Pacific and the Atlantic
oceans together with
global warming impact the risk
of drought and wildfire in southwestern North America.»
The
temperature and salinity
of seawater are key drivers for the
global ocean circulation system.
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 range
of pH and
temperature that some organisms experience on a daily basis exceeds the changes we expect to see in the
global ocean by the end
of the century,» notes Rivest, an assistant professor at VIMS.
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.
A detailed, long - term
ocean temperature record derived from corals on Christmas Island in Kiribati and other islands in the tropical Pacific shows that the extreme warmth
of recent El Niño events reflects not just the natural
ocean - atmosphere cycle but a new factor:
global warming caused by human activity.
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.
Climate models show the absence
of a
global atmospheric circulation pattern which bolsters high
ocean temperatures key to coral bleaching
These discoveries were made possible by the enhancement
of a
global network to monitor sea - surface
temperatures, under the auspices
of TOGA and another large international study, the World
Ocean Circulation Experiment.
«The mounting evidence is coalescing around the idea that decades
of stronger trade winds coincide with decades
of stalls or even slight cooling
of global surface
temperatures, as heat is apparently transferred from the atmosphere into the upper
ocean,» Linsley said.
In addition,
global sea level can fluctuate due to climate patterns such as El Niños and La Niñas (the opposing phases
of the El Niño Southern Oscillation, or ENSO) which influence
ocean temperature and
global precipitation patterns.
Scientists have discovered that rising
ocean temperatures slow the development
of baby fish around the equator, raising concerns about the impact
of global warming on fish and fisheries in the tropics.
Predicting the effects
of future
ocean warming on biogeochemical cycles depends critically on understanding how existing
global temperature variation affects phytoplankton.
Rising
ocean temperatures will alter the productivity and composition
of marine phytoplankton communities, thereby affecting
global biogeochemical cycles.
«The ability to adapt to changing conditions is going to become even more important as humans impact the environment, whether it's from
ocean acidification or increasing
temperatures or other types
of global changes that are occurring.»
The researchers paired MIT's
global circulation model — which simulates physical phenomena such as
ocean currents,
temperatures, and salinity — with an ecosystem model that simulates the behavior
of 96 species
of phytoplankton.
With records dating back to 1880, the
global temperature across the world's land and
ocean surfaces for August 2014 was 0.75 °C (1.35 °F) higher than the 20th century average
of 15.6 °C (60.1 °F).
With ENSO - neutral conditions present during the first half
of 2013, the January — June
global temperature across land and
ocean surfaces tied with 2003 as the seventh warmest such period, at 0.59 °C (1.06 °F) above the 20th century average.
It's the
ocean «These small
global temperature increases
of the last 25 years and over the last century are likely natural changes that the globe has seen many times in the past.
Surface
temperature is only a small fraction
of our climate with most
of global warming going into the
oceans.
This curve represents the portion
of global temperature that is not accounted for by the two main
ocean oscillations,
of respective periods 56 years and 75 years, and the CO2 blanket that Tyndall and Arrhenius wrote about in the 19th century.
The surface
ocean temperature is a large component
of the total
global temperature.
The observed and projected rates
of increase in freshwater runoff could potentially disrupt
ocean circulation if
global temperatures rise by 3 to 4 °C over this century as forecast by the IPCC 2001 report.