Limited to just detrended ENSO you are right, but there is that plowed under by CO2 assumptions secular trend, the pacific
centennial oscillation, that makes the difference.
Not exact matches
Reconstructed
centennial variability of Late Holocene storminess from Cors Fochno, Wales, UK Future anthropogenic climate forcing is forecast to increase storm intensity and frequency over Northern Europe, due to a northward shift of the storm tracks, and a positive North Atlantic
Oscillation.
The study by Macias & Johnson (2008) provides not only evidence for the link between decadal - scale changes in the teleconnection patterns (e.g. the Pacific Decadal
Oscillation (PDO) index) and the increased fire frequency in the late twentieth century but also an explanation of why the pattern of fire variability and fire - climate relationships changes at different time scales from
centennial / decadal to interannual.....
Off the Peruvian coast the ENSO
oscillation persists but with millennial,
centennial and millennial variations in the intensity and frequency of upwelling.
On the
centennial timescale, there was a +70 cm high level in the 16th and 17th centuries, a -50 cm low in the 18th century and a stability (with some
oscillations) in the 19th, 20th and early 21st centuries.
WHOI published on the
centennial scale Pacific
Oscillation which is also blissfully ignore and Toggwieler and Briereley have published on the impact of shifting westerlies and zonal / meridional temperature gradients also blissfully ignored.
Comparing decadal - with
centennial - scale «trends» in a process that contains important decadal - scale
oscillations is not an example of analytically robust science.
Superimposed on this trend are apparent dry — wet
oscillations at
centennial to millennial timescales most likely in response to solar activity.»
The speleothem documents multi-decadal to
centennial length
oscillations in δ18O that point to large variations in rainfall that have not been manifest in the short instrumental period.
Can long - term cycles in ocean temperature such as the Pacific Decadal
Oscillation explain the
centennial trend?
The temporal relationship between the Suess solar cycle and particularly significant 210 yr
oscillations in the speleothem δ18O records therefore supports the notion that solar variability played a significant role in driving
centennial - scale changes in the hydrological cycle in the subtropics during the Holocene.