As you can see in the chart below, the current normalised P / E ratio — which is used to strip out short -
term seasonal effects — is 19.2 for Europe.
Not exact matches
These month tables are useful for seeing longer
term trends —
seasonal ups and downs,
effect of publishing a new book, the
effect of the big changes in KDP algorithms etc..
Long -
term effects of warming and ocean acidification are modified by
seasonal variation in species responses and environmental conditions
A top - down climate
effect that shows long -
term drift (and may also be out of phase with the bottom - up solar forcing) would change the spatial response patterns and would mean that climate - chemistry models that have sufficient resolution in the stratosphere would become very important for making accurate regional /
seasonal climate predictions.
That is not to say that there may not be noticeable impacts on shorter
term measures — local and
seasonal trends and possibly daily temperature range (DTR)
effects for example.
These changes are intimately linked to species responses to
seasonal variations in environmental conditions (temperature and photoperiod) that, depending upon timing, can either exacerbate or buffer the long -
term directional
effects of climatic forcing.
Long -
term effects of warming and ocean acidification are modified by
seasonal variations in species responses and environmental conditions