Not exact matches
The four years
between planting a Kona tree and the first harvest extends
seasonal variations in the price of Kona.
Observations of atmospheric carbon dioxide made by aircraft at altitudes
between 3 and 6 kilometers (10,000 - 20,000 feet) show that
seasonal carbon dioxide
variations have substantially changed during the last 50 years.
Then, they looked at satellite data that measures
variations in Earth's gravitational field to track the long - term and
seasonal movements of water
between the oceans and the continents.
Ca
seasonal variation follows the behaviour expected from impact vaporization by interplanetary dust, due to Mercury's substantial radial excursions (heliocentric distances
between 0.306 AU at perihelion and 0.465 AU at aphelion).
The divergence
between fungal and bacterial communities in
seasonal and spatial
variations of wastewater treatment plants — Ziyan Wei — Science of The Total Environment
However, the relationship
between seasonal variation in body weight and
seasonal changes in caloric intake and physical activity, and in particular the relative importance of these factors in determining weight change, has not been as well studied.
FOR IMMEDIATE RELEASE David Baskin,
Seasonal Variations at Freight + Volume September 24, 2009 — October 31, 2009 / Reception: Thursday, September 24, 6 — 8 pm Negotiating the uncertain border
between the art object and consumerism, David Baskin's recent sculpture explores the underlying agendas inherent in the «formal» properties of everyday consumer goods.
Ice volume is estimated to be
between 1,000 and 4,000 km3 / yr and shows a large
seasonal variation.
For example, let's imagine that latitudinal and
seasonal variations (Milankovic) of insolation
between LGW and PI imply a + / -10 % of nebulosity, for some ocean - atmosphere circulation's reasons.
Even though such transitory influences as day and night or
seasonal variations in photosynthesis cause clearly visible swings in the curve, the 30 percent drop
between 1929 and 1932 caused not a ripple: empirical scientific evidence that the human contribution is in fact less than a fart in a hurricane, as Dr. Hertzberg says.
If one looks at the ocean / water temperatures http://weather.unisys.com/surface/sst.html there are enormous differences
between the tropics, temperate and north, and enormous
seasonal variations during the year which will affect CO2 absorption and emission, and there is a lot of biological activity in seas and waters that also are involved.
The 31 years of satellite measurement of OLR show an average OLR of around 232Watts / m ^ 2 with a range from 227Watts / m ^ 2 to 237Watts / m ^ 2 in response to the annual
seasonal variation in absolute global temperature
between 12 °C and 16 °C due to the significantly larger temperate landmass in the Northern hemisphere.
The relations
between the length of a solar cycle and the mean temperature in the following cycle are used to model Svalbard annual mean temperature and
seasonal temperature
variations.
A set of long, nearly complete daily precipitation series for Alaska spanning the latter half of the 20th century has been analyzed for
seasonal relationships
between variations in mean, heavy, and extreme precipitation and large - scale atmospheric circulation
variations at interannual, decadal, and secular timescales.
An examination of the data from: i) measurements of the fractionation of CO2 by way of Carbon - 12 and Carbon - 13 isotopes; ii) the
seasonal variations of the concentration of CO2 in the Northern Hemisphere; and iii) the time delay
between Northern and Southern Hemisphere
variations in CO2, raises questions about the conventional explanation of the source of increased atmospheric CO2.
Here we assess the diurnal and
seasonal variation of surface urban heat island intensity (SUHII) defined as the surface temperature difference
between urban area and suburban area measured from the MODIS.
The constancy of
seasonal variations in CO2 and the lack of time delays
between the hemispheres suggest that fossil fuel derived CO2 is almost totally absorbed locally in the year it is emitted.
Our own model would say
between 2040 and 2060, and it is fair to say that our view is that the earlier dates - in other words, the more pessimistic outlook for the Arctic - are associated with models that we believe are more credible, in terms of their capability to reproduce the observed
seasonal cycle in sea ice extent, and also the
variations in sea ice from year to year.
Seasonal response of BL cloud amount to SST
variations in oceanic subsidence regions
between 20 - 40 ° latitude