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  2. Sunspots (economics) - Wikipedia

    en.wikipedia.org/wiki/Sunspots_(economics)

    Experimental economics researchers have demonstrated how sunspots could affect economic activity. [ 7 ] The name is a whimsical reference to 19th-century economist William Stanley Jevons , who attempted to correlate business cycle patterns with sunspot counts (on the actual sun ) on the grounds that they might cause variations in weather and ...

  3. Convergence zone - Wikipedia

    en.wikipedia.org/wiki/Convergence_zone

    Large-scale convergence, called synoptic-scale convergence, is associated with weather systems such as baroclinic troughs, low-pressure areas, and cyclones. The large-scale convergence zone formed over the equator, the Intertropical Convergence Zone, has condensed and intensified as a result of the global increase in temperature. [2]

  4. Low-pressure area - Wikipedia

    en.wikipedia.org/wiki/Low-pressure_area

    Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere (aloft). The formation process of a low-pressure area is known as cyclogenesis . In meteorology , atmospheric divergence aloft occurs in two kinds of places:

  5. Convergence (economics) - Wikipedia

    en.wikipedia.org/wiki/Convergence_(economics)

    The idea of convergence in economics (also sometimes known as the catch-up effect) is the hypothesis that poorer economies' per capita incomes will tend to grow at faster rates than richer economies.

  6. Atmospheric convection - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_convection

    It stops rising when it has cooled to the same temperature as the surrounding air. Associated with a thermal is a downward flow surrounding the thermal column. The downward-moving exterior is caused by colder air being displaced at the top of the thermal. Another convection-driven weather effect is the sea breeze. [6] [7]

  7. Geostrophic wind - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_wind

    The geostrophic wind neglects frictional effects, which is usually a good approximation for the synoptic scale instantaneous flow in the midlatitude mid-troposphere. [4] Although ageostrophic terms are relatively small, they are essential for the time evolution of the flow and in particular are necessary for the growth and decay of storms.

  8. What is an Alberta clipper? - AOL

    www.aol.com/weather/alberta-clipper-213918845.html

    Residents of the Midwest, Plains, Great Lakes and Northeast may have heard of the term "Alberta clipper" when a winter storm is rolling through the region, but what is the meteorology behind the term?

  9. Divergence problem - Wikipedia

    en.wikipedia.org/wiki/Divergence_problem

    The divergence problem is an anomaly from the field of dendroclimatology, the study of past climate through observations of old trees, primarily the properties of their annual growth rings. It is the disagreement between instrumental temperatures (measured by thermometers ) and the temperatures reconstructed from latewood densities or, in some ...