Cool phase Pacific Decadal Oscillation winters are generally wetter and colder.
Not exact matches
El Nino and La Nina refer to the «warm and
cool phases of a recurring climate pattern across the tropical
Pacific,» according to the National Oceanic and Atmospheric Administration.
In April 2008, scientists at NASA's Jet Propulsion Laboratory announced that while the La Niña was weakening, the
Pacific Decadal Oscillation (PDO)-- a larger - scale, slower - cycling ocean pattern — had shifted to its
cool phase.
The
Pacific Ocean's current
cool phase is driving the global warming slowdown — but that countering effect is not going to last, scientists say.
During its positive
phase the ocean temperatures in the tropical
Pacific are unusually warm and those outside this region to the north and south are often unusually
cool.
Since the end of last El Niño warming event of 1997 to 1998, the tropical
Pacific Ocean has been in a relatively
cool phase — strong enough to offset the warming created by greenhouse gas emissions.
It has been in a
cool, La Niña - like
phase for 10 years, causing heat to sink deep into the
Pacific.
The recurring wave pattern of intense rain and thunderstorms, followed by a dry
phase as the force moves across the
cooler Pacific Ocean occurs every 30 - 60 days, giving this atmospheric wave its unique stamp on the climate.
Naturally occurring interannual and multidecadal shifts in regional ocean regimes such as the
Pacific El Niño - Southern Oscillation, the North Atlantic Oscillation, and the Atlantic Multidecadal Oscillation, for example, are bimodal oscillations that cycle between
phases of warmer and
cooler sea surface temperatures.
But, according to a new analysis in the journal Geophysical Research Letters by Ben Henley and Andrew King of the University of Melbourne, the 1.5 °C target may be reached or exceeded as early as 2026 if the Interdecadal
Pacific Oscillation (IPO) shifts sea surface temperatures in the
Pacific from a
cool to a warm
phase.
Plant drought - tolerant species in years with strong El Niño forecasts, particularly during
Pacific Decadal Oscillation warm
phase; plant trees that require sufficient water during establishment in La Niña years and during
Pacific Decadal Oscillation
cool phases Focus planting more in spring as fall planting becomes more difficult with reduced soil moisture and test different planting timings as springs shift earlier
The most influential cycles are the El Niño Southern Oscillation and the
Pacific Decadal Oscillation, which is a mighty cycle that typically takes 20 to 30 years to switch between its warm and
cool phases.
It's a pattern of ocean temperatures in the
Pacific that has a warm and
cool phase.
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
Pacific Decadal Oscillation and the Atlantic Multidecadal Oscillation have «fluttered» into their
cooling phase under the impetus of the
cooler sun.
A new paper by Andrew Dessler of Texas A&M University bolsters the established view of clouds» role as a feedback mechanism — but not driver — in climate dynamics through a decade of observation and analysis of El Nino and La Nina events (periodic warm and
cool phases of the
Pacific Ocean).
It's important to note that a substantial short - term influence on the globe's average temperature, the cycle of El Niño warmth and La Niña
cooling in the tropical
Pacific Ocean, was in the warm
phase until May but a La Niña
cooling is forecast later this year, according to the Climate Prediction Center of the National Oceanic and Atmospheric Administration.
Some highlights: Over part of the past year, the
Pacific was in its cyclical
cool phase, called La Niña; the Arctic remained far warmer than usual for recent decades.
This
cooling is the result of natural long - term swings in ocean surface temperatures, particularly swings in the Interdecadal
Pacific Oscillation or mega-El Niño - Southern Oscillation, which has lately been in a mega-La Niña or
cool phase.
The Jet Propulsion Laboratory of NASA recently reported that the
Pacific Ocean appears to be reverting to a
cool phase, as well.
The models overestimated warming from 1979 - 2011, but if you look at GISTEMP for example you can see that the East
Pacific is
cooler in 2011 than it was in 1979 and the models did not capture that as they have no PDO in the correct
phase and are not expected to because PDOs are transient changes.
In winter, the effect of the
cooler phase of the oscillation on the northern hemisphere is to depress temperatures slightly; but in summer, the
cooler waters in the equatorial
Pacific have less impact on the northern hemisphere's weather.
It was then called the Great
Pacific Climate Shift but since that time it has been subsumed into the PDO
phase shift from
cool to warm
phase that supposedly has a thirty year period.
The negative
phase of IPO is characterized by
cooler - than - average sea surface temperatures in the Eastern
Pacific, facilitating the expansion of Antarctic sea ice.
As seen in Figure 2, a
cool phase PDO is associated with
cool sea surface temperatures along the
Pacific coast of North America, but the center of the North
Pacific ocean is still quite warm.
Nor is anyone informed that during an earlier
cool phase of the
Pacific Decadal Oscillation, the droughts of the 1950s brought even less precipitation to the region, yet there was still greater river flow and less damage to the bay's fisheries.
The typical V of a
cool Pacific decadal
phase can be seen in the
Pacific with uprising of cold and nutrient rich water in both the north and south east.
For example, in the
Pacific, when easterlies increase in strength (as happens during the
cool phase of the PDO) the net surface may
cool but more heat is being sequestered at depth due to increased Ekman pumping, thus the net energy content of the ocean increases, even with a
cool surface layer.
Current «
cool»
phase of the PDO began in late 1998 / early 1999 (certainly not 2008), and when it flipped it generally meant
cooler sea surface temperatures along the west coast of N. America but warmer temperatures on average over other other broad regions of the
Pacific.
The
cool phase starts with upwelling which starts with flows in the Peruvian and Californian Currents spinning up with the
Pacific gyres.
The
cool phase PDO that the
Pacific also appears to be strengthening.
In 1976/77 the surface temperature of a vast area of the
Pacific Ocean abruptly warmed by several degrees as the
Pacific Decadal Oscillation shifted from «
cool phase» to «warm
phase».
The influence of the
Pacific Decadal Oscillation on instrumental and modeled Tsable River summer streamflow is likely linked to the enhanced role of snowmelt in determining summer discharge during
cool phases.
This occurred while the Equatorial
Pacific was flipped into a
cool phase, which tends to lower global temperatures.
«At the time of this writing (May 2010) the tropical
Pacific Ocean has changed from El Nino conditions to ENSO - neutral and is likely headed into the
cool La Nina
phase of the Southern Oscillation.
We are in a
cool phase of the
Pacific multidecadal variation — and the north - east
Pacific is
cooling.
The image below shows the
Pacific Ocean in the
cool phase of the
Pacific Decadal Oscillation (PDO) and the
cool phase (La Niña) of the ENSO.
«Many climatologists and astrophysicists believe recent sun spot,
Pacific Ocean and global temperature trends suggest that our planet may have entered a
cool phase that could last for 25 years.
I had previously noted that that the
Pacific has developed a
cool phase of the
Pacific Decadal Oscillation (PDO).
The new Jason oceanographic satellite shows that 2007 was a â $ œcoolâ $ La Nina yearâ $» but Jason also says something more important is at work: The much larger and more persistent
Pacific Decadal Oscillation (PDO) has turned into its
cool phase, telling -LSB-...]
John Philips (13:43:35) «Trends» have become virtually meaningless lately, since the word has been so variably used, but try this: Eyeball the temperature curve as correlated to the
Pacific Decadal Oscillation and you will see an excellent relationship with the cyclic
cooling and warming
phase of the PDO overlaid on a gradual warming trend emerging from the Little Ice Age.
kim (22:04:11): He also ignores the effect of a PDO in a
cooling phase, A
cool phase PDO leads to increased sea temperatures in the N
Pacific so you'd expect it to enhance melting.
The typical pattern of a
cool phase of the
Pacific decadal oscillation is for 20 to 40 years of more intense and more frequent La Nina.
However, an ENSO episode is a local release of heat stored in the South
Pacific Ocean into the atmosphere (or a local storing of heat causing the atmosphere to
cool during the opposite
phase).
On that basis I think we will see
cooling for a couple of decades due to the negative
phase of the
Pacific Decadal Oscillation which has just begun then at least one more 20 to 30 year
phase of natural warming before we start the true decline as the
cooler thermohaline waters from the Little Ice Age come back to the surface.
In 2011 we saw clear evidence of the warm pool in the
Pacific northwest (which is the main characteristic of the
cool PDO
phase) IS capable of «charging» the Walker Circulation pump that drives La Nina and inhibits El Nino.
Recent droughts are therefore not anomalous relative to the ~ 400 year pre-instrumental record... The influence of the
Pacific Decadal Oscillation on instrumental and modeled Tsable River summer streamflow is likely linked to the enhanced role of snowmelt in determining summer discharge during
cool phases.»
The implications of a
cool phase of the
Pacific Decadal Oscillation include a decades long and large increase in rainfall, cyclones and flooding in eastern and northern Australia.
The models heavily relied upon by the Intergovernmental Panel on Climate Change (IPCC) had not projected this multidecadal stasis in «global warming»; nor (until trained ex post facto) the fall in TS from 1940 - 1975; nor 50 years»
cooling in Antarctica (Doran et al., 2002) and the Arctic (Soon, 2005); nor the absence of ocean warming since 2003 (Lyman et al., 2006; Gouretski & Koltermann, 2007); nor the onset, duration, or intensity of the Madden - Julian intraseasonal oscillation, the Quasi-Biennial Oscillation in the tropical stratosphere, El Nino / La Nina oscillations, the Atlantic Multidecadal Oscillation, or the
Pacific Decadal Oscillation that has recently transited from its warming to its
cooling phase (oceanic oscillations which, on their own, may account for all of the observed warmings and
coolings over the past half - century: Tsoniset al., 2007); nor the magnitude nor duration of multi-century events such as the Mediaeval Warm Period or the Little Ice Age; nor the cessation since 2000 of the previously - observed growth in atmospheric methane concentration (IPCC, 2007); nor the active 2004 hurricane season; nor the inactive subsequent seasons; nor the UK flooding of 2007 (the Met Office had forecast a summer of prolonged droughts only six weeks previously); nor the solar Grand Maximum of the past 70 years, during which the Sun was more active, for longer, than at almost any similar period in the past 11,400 years (Hathaway, 2004; Solankiet al., 2005); nor the consequent surface «global warming» on Mars, Jupiter, Neptune's largest moon, and even distant Pluto; nor the eerily - continuing 2006 solar minimum; nor the consequent, precipitate decline of ~ 0.8 °C in TS from January 2007 to May 2008 that has canceled out almost all of the observed warming of the 20th century.
Girma Orssengo rightly demonstrates that one can not determine climate sensitivity empirically from observed changes in CO2 concentration and in global mean surface temperature unless one either studies periods that are multiples of ~ 60 years to cancel the transient effects of the warming and
cooling phases of the
Pacific and related ocean oscillations or studies periods centered on a
phase - transition in the ocean oscillations.