Sentence examples for timing of warming from inspiring English sources

We plan future work to model how the amount of warming, timing of warming and required GDDs may lead communities at different elevations to respond differentially to projected warming (see [59], [60]).

We also examined whether species that reach adulthood early versus late in the season differ in their degree of phenological advancement and whether this difference might be explained by the specific timing of warming.

[45], [46], [47]; but, as in other systems [6], it may also be attributed to the detailed seasonal timing of warming.

Our analyses provide clear evidence that variation in amount and timing of warming over the growing season explains the vast majority of phenological variation in this system.

In the following, we address the degree to which community-level phenological responses vary relative to the degree to which sites have warmed and the timing of warming.

This study thus illustrates that similar levels of warming (as measured by accumulated number of GDDs) can have very different impacts on species within communities according to the seasonal timing of warming and that the seasonal timing of warming and its effects on phenology can be year dependent (Figure 4).

The largest spatial variability in the timing of soil warming in spring between sites was found during years with little snow, which is a possible consequence of climate change-related warming in the boreal landscape of northern Sweden.

However, the timing of snowmelt and soil thaw, the onset of warming in the spring and other factors affecting phenology can have a large impact on the annual carbon balance in forests, in particular in cold climates [76, 77].

However, the timing of snowmelt and soil thaw, the onset of warming in the spring and other factors affecting phenology can have a large impact on the annual carbon balance in forests, in particular in cold climates [ 76, 77].

Over the past 25 years, the timing of this melting has become less predictable as a consequence of warming in the Arctic, varying by more than a month.

Differences in the timing of soil warming have been shown to influence the trees' capacity to take up water and assimilate carbon.