Not exact matches
«This indicates that we need to work with the
trees near the bottom of the mountain, because they are the ones that will feel the most stress from warming
temperatures,» Van Nuland said.
Studies of fossil
trees on a ridge of Mount Achernar in the Transantarctic Mountains
near the Ross Ice Shelf show that
temperatures in the region must have been warmer than they are today.
Many of the deepest branches in Woese's
tree, those that join
nearest to the three - way junction of the kingdoms, turned out to belong to organisms that live at high
temperatures, as in the fuming springs in Yellowstone Park or the volcanic vents that gash the ocean floor.
That's because South Padre Island, located
near the Mexico border, offers warm
temperatures, towering palm
trees, and stunning Gulf Coast beaches.
Chronologies developed from sites
near to the elevational or latitudinal
tree lines often show sensitivity to summer
temperature and, because of their annual resolution, absolute dating and relatively widespread nature, they have contributed to many local, continental and hemispheric
temperature reconstructions.
These
trees not only giving you shade and cooler
temperatures, but if placed
near your A / C unit, can help it run more efficiently.
Growth rates are sensitive to many things, this is why so much care is taken to select samples that one might rightly suspect will be highly sensitive to
temperature changes (such as
trees growing
near their altitudinal and latitudinal range extremes, which typically is due to the species limit of cold tolerance).
Its precisely because
temperature becomes the leading limiting fact at treeline that such locations have been used for past
temperature reconstructions, just like
trees growing
near their hydrological limits are chosen for drought reconstructions, etc..
This IS indeed possible for alpine treeline because the lateral scale of variation in
temperature is short and such a
near - neighbor comparison can be done between
trees near and distal from treeline.
For instance, in Briffa et a 2001 they talk about
trees being
near altitudinal or longitudinal limits being good candidates because range is limited by
temperature (not CO2 concentrations, or precip) and therefore relatively minor changes in
temperature cause a relatively larger change in growth rate than
trees growing in an area where conditions are more optimum.
The claim that
tree proxies kinda look like the actual
temperature for 40 or 60 years in the early 20th century if you are far away and
near sighted doesn't mean they are a «calibrated proxy».
``... large - scale
near - surface air -
temperature reconstructions relying on
tree - ring data may underestimate pre-instrumental
temperatures including warmth during Medieval and Roman times.»
Breitenmoser et al. (2012) analyzed the ~ 200 - year periodicity during the past two millennia using seventeen
near worldwide distributed
tree chronologies, and found significant periodicities in the 208 - year frequency band, corresponding to the DeVries cycle of solar activity, indicating a solar contribution in the
temperature and precipitation series.
Trees growing near to their ecological limits either in terms of latitude or altitude show growth limitations imposed by temperature and thus ring width variations in such trees contain a relatively strong temperature si
Trees growing
near to their ecological limits either in terms of latitude or altitude show growth limitations imposed by
temperature and thus ring width variations in such
trees contain a relatively strong temperature si
trees contain a relatively strong
temperature signal.
Trees growing near to the latitudinal or altitudinal treeline are mainly under growth limitations imposed by temperature and hence ring - width variations in such trees contain a strong temperature si
Trees growing
near to the latitudinal or altitudinal treeline are mainly under growth limitations imposed by
temperature and hence ring - width variations in such
trees contain a strong temperature si
trees contain a strong
temperature signal.
My mistake came in this sentence: «Yes, the effect of
temperature on
tree ring growth is likely to be an inverted quadratic, but that doesn't mean that local
temperature never gets
near the optimum or crosses over to the other side.»
cdquaries: Yes, the effect of
temperature on
tree ring growth is likely to be an inverted quadratic, but that doesn't mean that local
temperature ever gets
near the optimum or crosses over to the other side.
And as I used to see every summer, the combination of all of these factors means that the
trees up
near the treeline are often visibly stressed, branch tips turning brown, far into the downhill side of the inverse parabola, while
trees a few hundred metres lower were doing fine at essentially the same
temperature.
Thawing permafrost is also expected to alter area landscapes and make local ecosystems more susceptible to long - term damage, in part because permafrost degradation can lead to significant changes in local soil
temperatures and moisture levels.14, 20,21 Soils on or
near the banks of thermokarst ponds tend to be much drier than those on level tundra, owing to higher soil
temperatures and drainage.14, 20,21 On the Seward Peninsula, the banks of these ponds host
trees (usually spruces) and shrubs that are otherwise usually absent in the characteristically treeless tundra.14, 21
The City of Medford, while fulfilling its obligations for keeping river
temperatures down
near its White City wastewater treatment plant, is basically paying for the shady
trees that landowners along a five - mile stretch are planting.
At the precise moment when the
tree - ring proxies and actual
temperatures are in
near perfect agreement on a decades - long cooling trend, Mann dumps the
tree rings and moves to «observed
temperatures» - which have been conveniently revised upward from when they were originally observed.