Not exact matches
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Posted by Tony Zambito at 04:30 PM in buyer behavior, buyer decision
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Posted by Tony Zambito at 12:38 PM in buyer behavior, buyer decision
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Posted by Tony Zambito at 02:13 PM in buyer behavior, buyer decision
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Posted by Tony Zambito at 07:30 PM in buyer behavior, buyer decision
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The fact is that many of those «iterative»
models, where
content is developed using a
cycle of repeated processes, have proved immensely resilient over the years in projects that produced high - quality
content.
Therefore, we propose our enhanced TPACK
model as a series of semester - long
cycles that provide preservice teachers with multiple opportunities to experience the
content, pedagogy, and technology core tenets of the TPACK
model.
The climate
models as described here won't produce glacial / interglacial
cycles if run for a long time, and that is because they treat the atmospheric
content of trace IR - absorbing gases (CO2, methane and N2O) as external forcings.
It is a given that the existing
models do not fully incorporate data or mechanisms involving cloudiness or global albedo (reflectivity) variations or variations in the speed of the hydrological
cycle and that the variability in the temperatures of the ocean surfaces and the overall ocean energy
content are barely understood and wholly inadequately quantified in the infant attempts at coupled ocean / atmosphere
models.
Looking at the last decade, it is clear that the observed rate of change of upper ocean heat
content is a little slower than previously (and below linear extrapolations of the pre-2003
model output), and it remains unclear to what extent that is related to a reduction in net radiative forcing growth (due to the solar
cycle, or perhaps larger than expected aerosol forcing growth), or internal variability,
model errors, or data processing — arguments have been made for all four, singly and together.