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By contrast, mountains at temperate latitudes have strongly marked seasons.
At temperate latitudes, climates became progressively cooler, drier, and more seasonal.
But even at temperate European latitudes, scientists were finding plants moving north, new insects arriving and previously unseen diseases.
Since the mid-1990s, temperatures athehe northern pole have risen almost three times as much as they have at temperate latitudes.
Indoor house mice breed throughout the year, but outdoor populations at temperate latitudes breed only from early spring until late fall.
Weeds seem to benefit more than cereals at temperate latitudes, so they provide more competition to food crops for water, sunlight and nutrients.
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The maximum NEE occurred near T a = 30 °C at warm and humid summer sites, ~22 °C at continental temperate sites, and ~15 °C at a montane, semi-arid, and Mediterranean (US-Wrc) sites, except at the US-Blo (Mediterranean) site where it occurred at ~25 °C.
Both native and non-indigenous richness decreased with increasing copper concentrations at the tropical site whereas at the temperate site, non-indigenous richness was too low to detect any effect.
The ET increased alongside T a up to 33 35 °C at warm and humid summer sites, while it plateaued beyond 20 °C at continental temperate or montane, semi-arid, and Mediterranean sites, except at the US-Blo (Mediterranean) site where ET continued to rise with increasing T a up to 30 °C.
Sixty microliters of water were added to each well, incubated at room temperate for 2 min, and spun at 3220 g for 5 min. The concentration of the purified DNA was measured using a Nanodrop 8000 spectrophotometer (Thermo-Scientific), which ranged from 5 to 45 ng/μL.
Although the signal-to-noise ratio at room temperate is not as good as that at 80 K, three structures can still be clearly observed in the vicinity of 1.30, 1.34 and 1.36 eV, which can be assigned to the transitions of 1e1hh, 1e2hh and 1e1lh, respectively.
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