By
measuring changes in winds, rather than relying upon problematic temperature measurements, researchers estimated the atmospheric temperatures near 10 km in the Tropics rose about 0.65 degrees Celsius per decade since 1970 — probably the fastest warming rate anywhere in Earth's atmosphere.
By
measuring changes in winds, rather than relying upon problematic temperature measurements, Robert J. Allen and Steven C. Sherwood of the Department of Geology and Geophysics at Yale estimated the atmospheric temperatures near 10 km in the Tropics rose about 0.65 degrees Celsius per decade since 1970 — probably the fastest warming rate anywhere in Earth's atmosphere.
Not exact matches
The National Eclipse Ballooning Project, led by Angela Des Jardins, a solar physicist at Montana State University
in Bozeman, will launch over 100 weather balloons at various times along the path of totality and
measure changes in such parameters as temperature and
wind speed.
The images, taken over a 10 - hour period, created two massive maps of the entire planet, allowing scientists to
measure the speeds of Jupiter's
winds, identify different events
in its atmosphere, and track
changes in the outer layers of the planet.
They compared those events with
changes in the Global
Wind Oscillation (GWO) index, a collection of climate and weather information that
measures atmospheric angular momentum, or the degree of waviness
in the jet stream.
The analysis showed that
changes in cloud cover can serve as a proxy
in climate models for
wind velocity
in the atmosphere, which can not be directly
measured.
We will
measure how fast the streams flow, how turbulent they are, and how they respond to
changes in winds over the Southern Ocean.
Princen has also been known to reference scientific
measuring systems, mapping, and amateur anthropology
in his work, and his artistic practice has involved plotting ecological
changes — water currents,
wind patterns, and soil erosion, as well as the impacts of urban developments on the Dutch landscape.
Wind speed is a useful measure of storm strength (cat 1 - 5, (E) F scale...), and pressure drop also (~ wind speed * distance scale ~ speed * sqrt (area) if not too elongated)-- although (I think) potential energy ~ area * (change in p ^ 2) and kinetic energy ~ area * speed ^ 2 (assumes same vertical extent, density
Wind speed is a useful
measure of storm strength (cat 1 - 5, (E) F scale...), and pressure drop also (~
wind speed * distance scale ~ speed * sqrt (area) if not too elongated)-- although (I think) potential energy ~ area * (change in p ^ 2) and kinetic energy ~ area * speed ^ 2 (assumes same vertical extent, density
wind speed * distance scale ~ speed * sqrt (area) if not too elongated)-- although (I think) potential energy ~ area * (
change in p ^ 2) and kinetic energy ~ area * speed ^ 2 (assumes same vertical extent, density...)
As we have discussed elsewhere on this site, statistical
measures that focus on trends
in the strongest category storms, maximum hurricane
winds, and
changes in minimum central pressures, suggest a systematic increase
in the intensities of those storms that form.
2) There may be an increase of about 80 ppmv if one should
measure at exactly the same place as
in the 1940's at Poona
in exactly the same circumstances of
wind speed and other natural points (temperature, sunshine) and surroundings (no
change in urbanisation, energy use, cars, same crops
in the fields, same level of trees,...).
The concept is related to the more general phenomenon of climate
change, which refers to
changes in the totality of attributes that define climate — not only sur - face temperatures, but also precipitation patterns,
winds, ocean currents, and other
measures of the Earth's climate.
AER received a Business Achievement Award
in the climate
change category for developing new approaches and methods for
measuring and forecasting solar and
wind resources that allow renewable power plant developers to
measure more accurately both long - term production and short - term variations
in resource availability.
Mr Taylor has listed «
changes in building practices», «home solar water» and «household energy efficiency» as some
measures that are much cheaper options for reducing emissions than
wind energy.
Anders, the different behavior of the rising minimum could be due to increased moisture via El Ninos, land surface
changes that hold the morning heat when and where minimums are
measured,
changes in the
wind that lessen the pooling of cold morning air, or perhaps CO2.
Whether the large - scale thermodynamic environment and atmospheric static stability (often
measured by Convective Available Potential Energy, CAPE) becomes more favourable for tropical storms depends on how
changes in atmospheric circulation, especially subsidence, affect the static stability of the atmosphere, and how the
wind shear
changes.
Indeed, if it's not present
in BI, it may be that you only
wind up
measuring things you can't
change.
Suction blister
wounds are an excellent model for studying the effects of early
wound healing.50 Measurement of the rate of transepidermal water loss (TEWL) through human skin provides a noninvasive method to monitor
changes in the stratum corneum barrier function of the skin, providing an excellent objective method for evaluation of
wound healing.51 The 8 blister sites were assessed daily for 8 days following removal of the blister chambers50 and then again on day 12, along with daily control values from adjacent nonwounded skin; after subtracting the average control values from the average daily measurement, the 90 % standard for healing was based on reaching 90 % of the day 1
measures.