Posted by Richard
Primack
“A regular snowstorm has commenced,
fine flakes falling steadily, and rapidly whitening all the landscape. In half
an hour the russet earth is painted white even to the horizon. Do we know of
any other so silent and sudden a change?”
Henry David Thoreau, November 28, 1858
On February 6, the
Boston University Biogeosciences Program had a field trip to the Blue Hill Observatory, the longest running weather station in the United States. The Observatory was established in 1884 on a hill 10 miles south of Boston. We
often use data from the Observatory in our research to determine if long-term
phenological patterns are affected by temperature and rainfall. The Blue Hill Observatory is uniquely useful for our
purposes because its scientists have incorporated earlier weather observations
into their records, extending temperature data back to the 1830s and overlapping Henry David Thoreau’s phenology observations from Concord. For us, the key finding of the Observatory is that
the temperature of Boston has been getting warmer over the past 133 years.
The Blue Hill Observatory with weather instruments on top:
At the base of the Observatory, BU post-doc Eli Melaas explains the function and history of various
instruments. To his right is a designated spot that is regularly cleaned off to
record the amount of snowfall and the rate of snowfall:
This rain gauge has
a perimeter of flaps to create wind turbulence and create a more standardized
measure of precipitation. The Blue Hill Observatory is a pioneer in developing and
improving weather instruments:
On the roof of the Observatory, sunlight intensity is recorded when sunlight focused by the glass
ball burns holes in a standard paper sheet as the sun traverses overhead during
the course of the day:
A special feature of
the Observatory is that it uses both the original equipment and more modern
equipment in order to provide continuity in its measurements. Here are the
original barometers that are still used to record air pressure:
Wind speed from the
anemometers on the roof is recorded on a moving sheet of paper inside the Observatory: