There's a mantra in the trade that lower boundary treeline trees are precipitation proxies and
upper boundary tree lines are temperature proxies, relying on Lamarche 1974.
Not exact matches
The TMRCAs of major phylogenetic clades observed in the whole - exome
tree represent
upper boundaries for population split times.
As the elevational lapse rate of summer air temperatures in the Polar Urals is 0.7 °C, the climate - dependent
upper boundary of the zone suitable for
tree growth could ascend approximately 100 m.