``... The nearly 50 - yr time series shows that
the decadal change of the global oceanic evaporation (Evp) is marked by a distinct transition from a downward trend to an upward trend around 1977 — 78.
Real life suddenly interrupted data gathering, and all those sailors dipping their thermometers into buckets of wood or leather or steel checking for
that decadal change of a few hundredths of a degree that meant life or death for our planet suddenly had something else to worry about.
Changes in the watershed can, for example, lead to changes in alkalinity and CO2 fluxes that, together with metabolic processes and oceanic dynamics, yield high - magnitude
decadal changes of up to 0.5 units in coastal pH. Metabolism results in strong diel to seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily basis.
Not exact matches
This trade wind strengthening, which occurs during a the negative phase
of a phenomenon called the Interdecadal Pacific Oscillation (also known as the Pacific
Decadal Oscillation), pushes warm water westward and and
changes Pacific Ocean circulation.
Changes in the oceans occur more slowly than in the atmosphere, and this long - term memory
of the ocean is a major key to seasonal and
decadal predictions.
A new report by the National Academies
of Sciences, Engineering, and Medicine finds that continuity
of ocean observations is vital to gain an accurate understanding
of the climate, and calls for a
decadal, national plan that is adequately resourced and implemented to ensure critical ocean information is available to understand and predict future
changes.
The value
of this information is illustrated by the results
of a study published May 19 in the journal Geophysical Research Letters by Oster's group, working with colleagues from the Berkeley Geochronology Center, the Smithsonian Institution National Museum
of Natural History and the University
of Cambridge titled «Northeast Indian stalagmite records Pacific
decadal climate
change: Implications for moisture transport and drought in India.»
The working group on coupled biogeochemical cycling and controlling factors dealt with questions regarding the role
of plankton diversity, how ocean biogeochemistry will respond to global
changes on
decadal to centennial time scales, the key biogeochemical links between the ocean, atmosphere, and climate, and the role
of estuaries, shelves, and marginal seas in the capturing, transformation, and exchange
of terrestrial and open - marine material.
The study stops short
of attributing California's latest drought to
changes in Arctic sea ice, partly because there are other phenomena that play a role, like warm sea surface temperatures and
changes to the Pacific
Decadal Oscillation, an atmospheric climate pattern that typically shifts every 20 to 30 years.
Combining the STORM model with analysis
of the rainfall data set allowed the investigators to gain insights into
decadal trends in monsoonal rainfall intensity under climate
change.
April 23, 2018 - A new earth modeling system unveiled today will have weather - scale resolution and use advanced computers to simulate aspects
of Earth's variability and anticipate
decadal changes that will critically impact the U.S. energy sector in coming years.
There was also clear evidence
of decadal and multi-
decadal variability in the patterns
of change in MHW properties.
New research published this week in the Journal
of Climate reveals that one key measurement — large - scale upper - ocean temperature
changes caused by natural cycles
of the ocean — is a good indicator
of regional coastal sea level
changes on these
decadal timescales.
Figure 5: Contributions
of individual forcing agents to the total
change in the
decadal average temperature for three time periods.
Long - term (
decadal and multi-
decadal) variation in total annual streamflow is largely influenced by quasi-cyclic
changes in sea - surface temperatures and resulting climate conditions; the influence
of climate warming on these patterns is uncertain.
The first collection
of papers establishes that (a)
decadal and multi-
decadal ocean circulation patterns (AMO, PDO, NAO, ENSO) have significantly modulated precipitation and temperature
changes in recent decades, and the second collection
of papers confirm that (b) natural ocean oscillations are, in turn, modulated by solar activity.
In this study, we undertake another effort towards understanding the role
of the Sun in
changing or varying the Earth's climate on seasonal to
decadal time scale.
A number
of recent studies linking
changes in the North Atlantic ocean circulation to sea ice extent led Yeager to think that it would also be possible to make
decadal predictions for Arctic winter sea ice cover using the NCAR - based Community Earth System Model...
The rate
of release from the tundra alone is predicted to reach 1.5 billion tons
of carbon per annum before 2030, contributing to accelerated climate
change, perhaps resulting in sustained
decadal doubling
of ice loss causing collapse
of the Greenland Ice Sheet (Hansen et al, 2011).
«The impacts
of sea level
change will be felt most acutely during periods
of high sea level, both from this type
of interannual (and
decadal) variability as well as extreme events,» Church said.
From 1992 to 2003, the
decadal ocean heat content
changes (blue), along with the contributions from melting glaciers, ice sheets, and sea ice and small contributions from land and atmosphere warming, suggest a total warming (red) for the planet
of 0.6 ± 0.2 W / m2 (95 % error bars).
It is the top priority
of my research group to try to solve this problem to improve our climate predictions and, depending on the answer, it could affect predictions on all timescales from medium range forecasts, through monthly, seasonal,
decadal and even climate
change projections.
Figure 4: Contributions
of individual forcing agents to the total
decadal temperature
change for three time periods.
Hoerling and Kumar (2003) attributed the drought to
changes in atmospheric circulation associated with warming
of the western tropical Pacific and Indian oceans, while McCabe et al. (2004) have produced evidence suggesting that the confluence
of both Pacific
decadal and Atlantic multi-
decadal fluctuations is involved.
[11] Few attribute the decline in fog, and moreover, climate
change, to the Pacific
Decadal Oscillation, however, as the Pacific
Decadal Oscillation is an oscillation moving heat through the climate system but neither creating nor retaining heat, it is not a cause
of warming trends or declines in fog.
What is looked for is small
changes against a background
of large interannual variation to
decadal variation.
I focused on Fig 2
of Rahmstorf 2012, which shows the rate
of sea level
change in the form
of 10 yr
decadal trends.
Although I might not take it for granted that the horizontal homogeneity
of temperature due to the dynamic adjustment in the tropics would guarantee the horizontally uniform temperature
changes in the
decadal scale, the data do show it!
When I read the media PR on this, it looked like BEST claimed better statistical methods, leading to lower estimates
of the uncertainty in the temperature
change - even at the
decadal level.
There is even evidence
of annual -
decadal heat content
changes down to 1500 meters.
Mike's work, like that
of previous award winners, is diverse, and includes pioneering and highly cited work in time series analysis (an elegant use
of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations in the climate record and methods for smoothing temporal data),
decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth
of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST
changes, a finding recently reaffirmed by a study published in Nature), in showing how
changes in radiative forcing from volcanoes can affect ENSO, in examining the role
of solar variations in explaining the pattern
of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate
changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit
of work in atmospheric chemistry (an analysis
of beryllium - 7 measurements).
For the Earth's «fast» system,
changes in
decadal statistics can be computed on the basis
of changes in forcing such as GHG's, without any need for knowledge
of the initial conditions.
Thermal mass
of the oceans on the other hand is huge, so they follow with some principal lag
of decades, but they follow «noisy» as
decadal variations like ENSO or
changes in weather patterns due to climate
change overlay that.
It also hasn't been well - argued that there is a need to replace the underlying framework we have
of how climate
changes on
decadal timescales.
The rate
of increase (i.e.
change in temperature per year) is increasing, so maybe the best way to tell is by comparing
decadal changes.
If you can't keep up with annual -
decadal changes in the TOA radiative imbalance or ocean heat content (because
of failure to correctly model
changes in the atmosphere and ocean due to natural variability), then your climate model lacks fidelity to the real world system it is tasked to represent.
This is important because * if * resources were more abundant and * if * climate
change were happening more slowly and * if * climate could not possibly
change multiple degrees and multiple meters
of SLR on
decadal time scales, my solution set would be vastly different.
Bob Davis also won the AAG Climate Specialty Group Paper
of the Year award in 2004 for his paper «
Decadal changes in summer mortality in U.S. cities,» International Journal
of Biometeorology 47:166 - 175.
Northeast Pacific coastal warming since 1900 is often ascribed to anthropogenic greenhouse forcing, whereas multidecadal temperature
changes are widely interpreted in the framework
of the Pacific
Decadal Oscillation (PDO), which responds to regional atmospheric dynamics.
While rereading the ocean heat content
changes by Levitus 2005 at http://www.nodc.noaa.gov/OC5/PDF/PAPERS/grlheat05.pdf a remarkable sentence was noticed: «However, the large decrease in ocean heat content starting around 1980 suggests that internal variability
of the Earth system significantly affects Earth's heat balance on
decadal time - scales.»
Back around 2007/8, two high - profile papers claimed to produce, for the first time, skilful predictions
of decadal climate
change, based on new techniques
of ocean state initialization in climate models.
When this reinforces the anthropogenic
change, it can cause RILEs [rapid ice loss events]-- but it can also counter that
change and cause brief periods
of near - stability (or even small increases on a
decadal scale).
Next point,
changes in volcanic activity can affect
decadal and century - scale temperatures due to the random occurence
of eruptions
of the right sort (though I don't think you dispute that).
These factors driving the present
changes of the NHSM system are instrumental for understanding and predicting future
decadal changes and determining the proportions
of climate
change that are attributable to anthropogenic effects and long - term internal variability in the complex climate system.
Concerning climate -
change forecasting, we can not expect that increased computer power and improved climate models will in the future «give more precise probability distributions
of outcomes at the regional and
decadal scales».
The declining signal over India shown by the GPCP
decadal mode is broadly consistent with gauge measurements since the 1950s — that several research groups including my own are trying to understand, perhaps relating to emissions
of anthropogenic aerosol — although there are discrepancies between these gauge - based data sets themselves (see our recent review in Nature Climate
Change, for example).
On
decadal and longer time scales, global mean sea level
change results from two major processes, mostly related to recent climate
change, that alter the volume
of water in the global ocean: i) thermal expansion (Section 5.5.3), and ii) the exchange
of water between oceans and other reservoirs (glaciers and ice caps, ice sheets, other land water reservoirs - including through anthropogenic
change in land hydrology, and the atmosphere; Section 5.5.5).
The likelihood
of climate -
change catastrophe obviously is zero on
decadal time - scales, and it is reasonably small too (we hope!)
«Contributions
of Stratospheric Water Vapor to
Decadal Changes in the Rate
of Global Warming.»
Using the figures from the table, the
change in average «
decadal» TOA flux (with,
of course, only 9 years for the final «decade») are: