Sentences with phrase «soi index»

The SOI index has recently spiked pointing to a stronger La Nina to come.
I think those estimates overestimate the ENSO contribution by not using the SOI index, but that is neither here nor there.
For example, in 2009, the SOI Index was -0.12 (CPC index), the Nino 3.4 Index was 0.471, the AMO index was 0.073, the PDO Index was -0.613.
Can you confirm or correct me in the following: The SOI line is a function of a trend (eg extra CO2 forcing) plus some function of the SOI index and volcanic forcing
What is even more remarkable, is the fact that common frequencies seen in the two data sets [i.e. the flux optical depth anomaly and the SOI index] are simply those that would be expected if ENSO phenomenon is a resonant response of the Earth's (atmospheric / oceanic) climate system brought about by a coupling between it and the Earth's forced (18.6 year Nodical Lunar Cycle) and unforced (1.2 year Chandler Wobble) nutations.
Positive SOI index values, on the other hand, describe cold - phase or La Niña - like conditions and a southwestward displacement of the SPCZ.
Negative SOI index values are associated with warm - phase or El Niño - like conditions and a northeastward displacement of the SPCZ.
He based his main skeptical ideas on the SOI index — which is ironically causally about CO2 coming out of solution in the Pacific, to one side or the other, and impacting surface conductivities associated with the capacitive couplings I am writing about that change cloud microphysics.
There was nothing special about 2012 conditions to have caused a big dip (e.g. SOI index didn't show any big El Niño events over the year).

Not exact matches

The Southern Oscillation Index (SOI) is a measure of La Niña.
This figure from the McLean et al (2009) research shows that mean monthly global temperature (MSU GTTA) corresponds in general terms with the Southern Oscillation Index (SOI) of seven months earlier.
It should be noted that detrended data was used purely to establish the time lag between the Southern Oscillation Index (SOI) and MGT in Figures 5 and 6.
Time series for the Southern Oscillation Index (SOI) and global tropospheric temperature anomalies (GTTA) are compared for the 1958 − 2008 period.
To remove short - term noise, they plotted a 12 month running average of Global Tropospheric Temperature Anomaly (GTTA, the light grey line) and the Southern Oscillation Index (SOI, the black line).
The Southern Oscillation Index (SOI) is an indicator for the development of the easterly trade winds at the equatorial Pacific and thus tells us what's ahead for the ENSO.
Another interesting feature of McLean et al 2009 is a plot of unfiltered temperature data (GTTA) against the Southern Oscillation Index (SOI) to illustrate the quality of the match between them.
If some soi - disant index funds «aren't,» which ones «are» — or, at the most basic level, what is an index?
The Southern Oscillation Index (SOI) is indirectly based on temperature.
Reliable data on decadal variability of the Earth's radiation budget are hard to come by, but to provide some reality check I based my setting of the scaling factor between radiative forcing and the SOI / PDOI index on the tropical data of Wielecki et al 2002 (as corrected in response to Trenberth's criticism here.)
Based on this estimate and on the typical magnitude of Spencer's combined SOI / PDOI index, I chose a scaling factor (Roy's a) of 0.27 W / m2..
He took two indices of interannual variability: the Southern Oscillation (SOI) index, which is a proxy for El Nino, and the Pacific Decadal Oscillation Index (Pindex, which is a proxy for El Nino, and the Pacific Decadal Oscillation Index (PIndex (PDOI).
The analyses from SOI, Nino 3 index and GCM's are all comparable.»
A combination of vertical and horizontal excitation in forcing could certainly lead to the quasiperiodicity seen in the ENSO indices such as SOI.
A classic example is the Southern Oscillation (SO), encompassing the entire tropical Pacific, yet encapsulated by a simple SO Index (SOI), based on differences between Tahiti (eastern Pacific) and Darwin (western Pacific) MSLP anomalies.
It finds that the Southern Oscillation Index (SOI)-- the basic tool for forecasting variations in global and oceanic patterns — and rainfall fluctuations recorded over the last decade are similar to those in 1914 -1924.
The Southern Oscillation Index (SOI) is a metric for describing warm - and cold - phase conditions associated with the El Niño — Southern Oscillation (ENSO) and can also describe movements of the position of the SPCZ.
30 - day SOI values for the past two years Select to see full - size map of 30 - day Southern Oscillation Index values for the past two years, updated daily.
The 30 - day Southern Oscillation Index (SOI) to 11 March was +3.2 (90 - day value +0.9), which is within the neutral range.
Other ENSO indicators such as the Southern Oscillation Index (SOI) and tropical cloud patterns have persisted at neutral levels since late July.
El Niño is defined by SST anomalies in the eastern tropical Pacific while the Southern Oscillation Index (SOI) is a measure of the atmospheric circulation response in the Pacific - Indian Ocean region.
The Pacific and Atlantic Ocean temperature oscillations as measured by the PDO, ENSO, SOI, AMO, ETC indices are prime drivers of our climate.
The SOI (southern oscillation index) is also spiking up again this month, which argues against the bottoming out of the current La Nina.
Rather than define a somewhat arbitrary threshold for a La Niña / El Niño year (i.e. based on the size of the index and number of months exceeding a certain threshold) or limiting the analysis to one ENSO index, I first took the average of the three indices mentioned above (ONI, MEI, and SOI, accounting for the fact that positive SOI indicates La Niña conditions while the opposite is true for ONI and MEI).
And what about the other indices that are indicative of changes in the El Niño Southern Oscilation (ENSO), like the Multivariate ENSO Index (MEI) and Southern Oscillation Index (SOI)?
And so someone finally comes along and actually applies the Southern Oscillation Index (SOI) to compensate for the noise and we learn that these excursions are ALWAYS overtaken by further secular warming.
The Southern Oscillation Index (SOI) is calculated from the monthly or seasonal fluctuations in the air pressure difference between Tahiti and Darwin.
They also tried using Southern Oscillation Index (SOI) data for ENSO, sunspot number data for solar activity, and a volcanic radiative forcing reconstruction from Ammann et al. (2003), but found these changes made little difference to their results:
The SOI (southern oscillation index) is high.
I do a variation of this by subtracting out the Southern Oscillation Index (SOI) from the GMST profile, which effectively removes the pause / hiatus, leaving the underlying warming trend in its wake:
I know what it shows, a variation due to the SOI, an index which has been stationary and virtually trendless for the last 130 + years.
You have two indices, GST and SOI.
The ENSO cycle as described by the Southern Oscillation Index (SOI) perfectly captures the last 15 year pause.
This correction is conveniently provided by the Southern Oscillation Index (SOI), which shows no long - term bias.
All three major indices the PDO, AMO and SOI / ENSO appear to have in common a decadal modulation process caused by the natural sources as displayed here: http://www.vukcevic.talktalk.net/A&P.htm More info on my data will be available soon.
Hi Willis, Your fig 3 seems to bear some kind of relationship (not perfect but clearly related) to the southern oscillation index SOI
The current pause is explained as a compensation of increasing temperatures by a fortuitous sequence of cooling Pacific events as documented by the ENSO index, SOI.
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