Not exact matches
The rings formed in tree trunks during trees»
growth periods are valuable repositories of environmental information: the ring width reflects the tree's
growth conditions, which are a combination of the
temperature, precipitation and nutrient conditions during a given growing
season.
But warmer
temperatures, longer growing
seasons, and thawing permafrost (which supplies nutrients) are also promoting the
growth of aquatic plants in the ponds, shrinking the size of the basins.
«Other variables, including
temperatures during the rest of the growing
season in July and August, barely had an impact on shrub
growth.»
Microscopic imaging reveals the pattern of annual rings in shrub stems, which the researchers used to determine that shrub
growth is controlled by
temperatures in June, the first month of the brief arctic growing
season.
«Combined with warmer ocean
temperatures throughout the year, this leads to a longer growing
season and faster plankton
growth rates.
In physical geography, tundra is an area where the tree
growth is hindered by low
temperatures and short growing
seasons.
Warming
temperatures, increased atmospheric CO2, and longer growing
seasons provide opportunities for increased photosynthesis, thereby improving forest
growth and productivity (Ehleringer and Cerling 1995; Joyce and Birdsey 1995; Waring and Running 2007; NPS 2010).
They measure
growth, which can be affected by rainfall,
temperature, growing
season length, etc..
These rings form when
temperatures drop well below freezing for extended periods during the tree's growing
season, and are evidenced by physical scarring of that year's
growth ring that can be caused by volcanically induced climate dislocation — an idea first suggested by LaMarche and Hirschboeck in 1984.
Yet our prediction is that all trees within a region of synoptic or lesser scale where growing
season temperatures lie below the
growth threshold will experience a missing ring.
The attenuation of the response is produced primarily by the loss of sensitivity to further cooling for eruptions that place growing
season temperatures close to the lower threshold for
growth.
This is data linking
temperature with pollen count, how do we know that the increase of
temperature is not causing the increase in pollen count (increased land available for
growth, longer growing
seasons, etc)?
Other in situ and satellite data suggest that even though the seasonal ice cover was formed later in the fall of 2007, the mean thickness of first year ice cover is comparable to that of the previous two
seasons because of lower snow accumulation and lower air
temperatures and thus, faster
growth.
Changes in proxy records, either physical (such as the isotopic composition of various elements in ice) or biological (such as the width of a tree ring or the chemical composition of a
growth band in coral), do not respond precisely or solely to changes in any specific climate parameter (such as mean
temperature or total rainfall), or to the changes in that parameter as measured over a specific «
season» (such as June - August or January - December).
While their conservative physiology — retention of needles for one to several decades — provides a buffer to year - to - year changes evident in the high autocorrelation of ringwidth series, the critical factors limiting
growth are growing -
season length and mean
temperature over that period.
Plus, warmer spring
temperatures may increase the
growth of certain types of mold, further worsening the
season for allergy sufferers.
The researchers also discovered that a
temperature that is only three degrees Celsius warmer increased the dispersal of seeds and the speed at which populations spread throughout the
growth season.
These could be high winds, high
temperatures and drought, and, in desert regions, unusually high rainfall the preceding
season that triggers greater
growth and more fuel for the next fire.
Changes in proxy records, either physical (such as the isotopic composition of various elements in ice) or biological (such as the width of a tree ring or the chemical composition of a
growth band in coral), do not respond precisely or solely to changes in any specific climate parameter (such as mean
temperature or total rainfall), or to the changes in that parameter as measured over a specific «
season» (such as June to August or January to December).
For TRW, forcing is dominated by July
temperatures of the current year of
growth while MXD has a significant positive response to June, July and August
temperatures of the current growing
season.
However, when the new Torneträsk data is analysed using a regional
temperature record representing a large area in northern Sweden, there is a significant
growth response to an extended five - month summer
season, including also April and May (Fig. 7), thus confirming the results from Briffa et al. (1990) who found a significant correlation with April — August
temperatures using gridded (5 ° × 5 °)
temperature data for northern Fennoscandia.
I'm looking forward to the explanation of why temperate and boreal trees» primary and secondary meristems go dormant during the cold
season (= no
growth) but those of tropical trees, which have no such
season, do not, and why ITRDB tree ring data at
temperature limited sites show such suspiciously high correlations between the
growth rates of the different trees in a stand.
«Along with an increase in
temperatures, the spring
season also brings out the buyers and an increase in demand to the housing market, which most often translates to faster price
growth and a decrease in marketing times,» says Alex Villacorta, vice president of Research and Analytics at Clear Capital.