Therefore, there are reasons to expect that there has been a downward trend in moist stability in the Atlantic over the past few decades, independent of the reliability of
the tropical mean trend in the reanalysis.
Not exact matches
No, you are wrong, RSS is consistent with models only if we look at global
trends, but RSS
trend for
tropical «hot - spot» is out of 2 standard deviations limit of the model
mean, just like UAH and all «uncorrected» radiosonde data sets.
Wong et al. 2006 find for example an upward
trend (decrease of outgoing SW) for the
mean tropical zone, but with no information on the regional signature of this
trend.
doi: 10.1002 / joc.1651 (Not quoted in SOD) note «Model results and observed temperature
trends are in disagreement in most of the
tropical troposphere, being separated by more than twice the uncertainty of the model
mean.»
Figure 1 Vertical profile of
tropical mean temperature
trends.
It seems to me, that as the number of models grows this converges to a test as to whether the model
mean falls within the CI of the observed series
trend (which is pretty wide for the
tropical troposphere).
Since the
tropical oceans have flattened out and solar does have its largest impact on the
tropical oceans, I would expect about the same possibly some increase in Arctic sea ice over the next decade Not a consistent increase by any
means, but I doubt it will make it to the 2 mkm ^ 2 and will
trend towards a 6 million km ^ 2 average which is hardly «ice free».
The CMIP3 models show a 1979 — 2010
tropical SST
trend of 0.19 °C per decade in the multi-model
mean, much larger than the various observational
trend estimates ranging from 0.10 °C to 0.14 °C per decade (including the 95 % confidence interval, (Fu et al., 2011)-RRB-.
The results here reveal a larger picture — that the western
tropical Indian Ocean has been warming for more than a century, at a rate faster than any other region of the
tropical oceans, and turns out to be the largest contributor to the overall
trend in the global
mean sea surface temperature (SST)»
We found that relative to the global -
mean trends of the respective layers, both hemispheres have experienced enhanced tropospheric warming and stratospheric cooling in the 15 to 45 ° latitude belt, which is a pattern indicative of a widening of the
tropical circulation and a poleward shift of the tropospheric jet streams and their associated subtropical dry zones.
While global
mean temperature and
tropical Atlantic SSTs show pronounced and statistically significant warming
trends (green curves), the U.S. landfalling hurricane record (orange curve) shows no significant increase or decrease.