This inefficiency will increase as the product temperature and
temperature difference between the product and steam reduces.
Not exact matches
At a particular location within the
product, a local freezing rate can be defined as the ratio of the
difference between the initial
temperature and desired
temperature to the time elapsed in reaching the given final
temperature (Persson and Lohndal, 1993).
Differences between the
temperature anomaly
products is related to: different selections of input data, different methods for assessing urban heating effects, and (most important) different methodologies for estimating
temperatures in data - poor regions like the Arctic.
My attention was drawn in August to a draft version of a paper by Phil Klotzbach and colleagues that discussed the
differences between global
temperature products.
Sampling biases are easy to see in the
difference between the GISTEMP surface
temperature data
product (which extrapolates over the Arctic region) and the HADCRUT3v
product which assumes that Arctic
temperature anomalies don't extend past the land.