World View of Global Warming
Global Warming in the Temperate Zone
Copyright © 2005 - 2008
Pushing the Boundaries of Life: Mid-latitudes
The myriad creatures and plants with whom we share this planet are intimately
tied to their habitat and zone of temperature, precipitation or ocean
current. As mean temperatures rise, and climate is affected, living things
have no choice but to react -- to move or adapt. On earlier pages, this
Web site documents some of these changes in polar regions, where climate
change is very dramatic
The same changes are at play in the mid latitudes, also. It is
very clear that huge changes in biodiversity and individual creatures
are happening now -- and are accelerating.
In the past few years, scientists have published a large number
of studies showing strong correlations among animal and plant range changes.
The latest of these were published in January 2003 and 2004 in the
journal Nature.
In the latest of these far-reaching peer-reviewed articles, an
international group of scientists has predicted that by mid century up
to a third of land plants and animal species may be pushed close to extinction.
The study, "Extinction risk from climate change," measured the
responses to current change and habitat limits of 1103 species in many
habitats, and found that climate change is "...likely to be the greatest
threat in many if not most regions."
A year before, Nature published an analysis of studies of more than 1,700
species indicating significant range shifts averaging 6.1 km per decade
towards the poles. It reported that natural springtime events
are occurring earlier by 2.3 days per decade in the late 20th century.
A second analysis of 143 studies shows a significant impact of global
warming is already discernible in animal and plant populations.
See my Reference section for details of many such studies. Photos of some
plant and animal reactions in the temperate zone are the subject of this
portion of World View of Global Warming..
Pushing the Boundaries of Life: Temperate Zone
Alpine
meadow and fell-field ecosystems are changing under atmospheric warming.
On this site at 3000 meters in the Austrian Alps, Botanist Harald Pauli
and researchers are finding plant species increasing and decreasing at
different rates over a 10 year period. Essentially, the familiar
alpine wildflower fields are being fragmented and rearranged. This
is especially dangerous for plants forced to move upwards where there
is just rock and ice, says Pauli. "We are running into a really
serious loss of biodiversity." The 380 sites here were established
in 1994 by Georg Grabherr, Pauli and others at the University of Vienna.
This alpine research idea has expanded world wide into GLORIA - the "Global
Observation Research Initiative in Alpine Environments."
The glaciers behind the scientists are an even more visible sign of global
warming, and have receded many meters per year recently.
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Marine Biologist Rafe Sagarin points out some of the tide pool
habitat that was found to have changed when he re-inventoried a
60-year-old study at Hopkins Marine Laboratory, Monterey California.
Summer sea temperature has risen more than one degree in that time,
and the re-survey showed many warm water tidepool animals had increased
while those favoring colder water had decreased. |
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This nudibranch Hopkinsia rosea, discovered at and named
for the Hopkins Lab, was numerous in the 1930s survey but not seen
at all 60 years later. It is still found in other locations near
Monterey, favoring cooler water. Other species, such as predatory
snails and anemones showed great shifts in those thriving in warmer
water south on the California coast. |
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series of observations of even longer duration shows changes in
distribution and abundance of zooplankton and intertidal life in
the western English Channel. With data going back 70
years from the Marine Biological Association lab in Plymouth England,
this study by Alan Southward, Stephen Hawkins and M. T. Burrowsc
clearly tracks the effects of rising temperatures. The distribution
of both plankton and tidepool organisms was shifted up to 120 miles,
and there were increases or decreases of 2 to 3 orders of magnitude
in abundance. Warm water species increased in abundance and
extended their range during periods of warming, while cold-water
species declined or retreated. Underlining the sensitivity
of these ocean creatures is data showing that the reverse movement
occurred during a period of cooling in the mid-20th century.
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| Biologist
Camille Parmesan compared old records of the Ediths checkerspot
butterfly against current habitat from Mexico to Canada and found
that the insect had moved its habitat slightly north in response
to climate warming. She found the level of population extinctions
is four times as high at the far southern end of the range (Mexico)
than at the northern. This change in a sensitive insect was predicted
from the twentieth century warming of about 1 degree F.
The butterfly pictured is laying eggs on Collinsia, an annual
plant of Sierra Nevada high meadows. Annual plants are more
affected by weather shifts, and this is one of the factors in the
butterfly population shifting as climate changes the habitat of
both animals and their host plants.
Dr.
Parmesan later collaborated with many European biologists and lepidopterists
to show that 2/3 of butterfly species with long observational records
had shifted northward by from 22 to 150 miles, consistent with temperature
increases in Europe. No butterflies were found to have shifted
to the south. Parmesan has found many locations in Southern
France with apparently intact food-plant habitat that no longer
have well known butterflies like the Apollo (Parnassius apollo)..
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Throughout the temperate zone, changes are being recorded in where
and when plants bloom and thrive. One recent study by botanists
at the Smithsonian's National Museum of Natural History reviewed
records on the spring bloom time of 100 common Washington D.C. area
plants. Eighty-nine of the 100 showed significantly earlier blooming.
This one, the common lawn weed deadnettle, photographed at the National
Arboretum, is blooming an average of 39 days earlier than in 1970.
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American ornithologists are investigating climate change in several
ways. Jeff Price of the American Birding Congress collects data
from birders and scientists and reports changing migration and ranges
for hundreds of North American species. This yellow warbler was
an early migrant at Point Pelee National Park, Ontario. |
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Meanwhile Terry Root of Michgan University correlated
regional temperatures with a 50 year record of bird arrival at Seney
National Wildlife Refuge, Michigan. Comparing yearly records kept
by now-retired field biologist Elizabeth Losey with current arrival
times showed significantly early in-migration.
Even though the predicted range of climate warming has just begun,
many ecologial responses are already clearly visible, as seen in
these and other studies. Recent scientific reviews of biologial
research show that strong effects are being seen in habitats from
alpine meadows to coral reefs, and from the tropics
to the poles.
Among the important review articles are Gian-Reto Walther et al.,
"Ecological responses to recent climate change." Nature
416 (28 March 2002), and Drew Harvell et al., "Climate Warming
and Disease Risks for Terrestrial and Marine Biota," Science
296 (Jun 31 2002). World View of Global Warming will be documenting
some of these studies in the coming months.
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Tree swallow Tachycineta bicolor in nest hole at Point Pelee, Ontario
Another study showed the egg laying date of North American tree
swallows advanced by up to nine days during the period from 1959
to 1991. Reported in 1999 by Peter O. Dunn, Univ. of Wisconsin and
David W. Winkler, Cornell Univ, the research correlated 3450 nest
records, taking into account differences of location, elevation
and other breeding factors. "WE conclude," wrote the scientists,
"that tree swallows across North America are breeding earlier
and that the most likely cause is a long term increase in spring
temperature."
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Mountains
are undergoing some of the most crucial changes due to global warming.
Besides the loss of glaciers,
warming temperatures are driving the alpine zones farther up toward
the summits. Eventually, the highest alpine plants and animals
will have nowhere to go. This effect is being seen in and
near Rocky Mountain National Park, where marmots are coming out
of hibernation earlier, and in Great Basin mountains where some
populations of pikas have disappeared apparently due to climate
changes.
Other
research is focused on alpine trees and meadows, showing that mountain
hemlocks and sub alpine firs are moving into meadow areas in Mt
Rainier and Olympic National Parks -- and the effect is expected
to accelerate if temperatures continue to rise rapidly. In
Yellowstone National Park, the zone of life for the whitebark
pine is moving up toward the summit of the mountains. If this
reduces the number of these pines, it will affect not merely scenery,
because the seeds of the whitebark are a crucial part of grizzly
bear diet.
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"Sez who?": References 4
Each of the foregoing photos reports on documented science,
peer-reviewed published studies and scientific literature surveys. Those
references are listed later in this Web site, along with climate change
data, World View of Global Warming project advisors, and links to some
sources of climate information.
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