Geoscience Reference
In-Depth Information
Timing of flood (F) and drought (D) in North America, northern China, Patagonia, the Nile valley, India and the coincidence with the
18.6 year lunar tide
Table 2.2
Lunar
Canadian
United States
N. China
Patagonian
Nile in
India
Maxima
Prairies
Great Plains
Andes
Africa
1583
1581D
1582D
1601
1601D
1600D
1606F
1620
1622D
1620D
1621F
1638
1640D
1640D
1637F
1657
1652F
1659D
1656F
1676
1674F
1678D
1675F
1694
1694F
1693F
1713
1712F
1710F
1713D
1731
1729F
1727F
1733D
1750
1752F
1752D
1750D
1768
1768F
1768D
1766D
1787
1786F
1784D
1789D
1806
1805F
1805D
1806F
1802D
1806D
1824
1823F
1824D
1823F
1822D
1822D
1843
1843F
1844D
1846D
1841D
1837D
1861 1859F 1861D 1862D 1864D
1880 1881F 1879D 1881D 1880D 1885D
1899 1900F 1901D 1900D 1895D 1902D 1902D
1918 1916F 1919D 1918D 1918F 1917F 1913F
1936 1932F 1935D 1935F 1937F 1936F 1939F
1955 1953F 1955D 1954F 1956F 1953F 1958F
1973 1975F 1975D 1974F 1973F 1975F 1976F
1991 1995F 1993F 1990F 1992F 1996F 1990F
Sources: Currie (1984) and various internet searches. Since 1980, plotted rainfall anomalies for each region using
http://climexp.knmi.nl/fieldplot.cgi?someone@somewhere+gpcp
CONCLUDING COMMENTS
hazards, the realization is that they represent insepa-
rable hazards that follow each other in time as night
does day. Not only are the two events linked, but their
occurrence is also remarkably coincident across the
globe. They are intricately connected to the Southern
Oscillation and other spatial cyclic phenomena such as
the North Atlantic and North Pacific Oscillations.
Other hazards - such as tropical and extra-tropical
cyclones, wave erosion, and land instability - are
also correlated to the Southern Oscillation, and thus
subject to prediction. At mid-latitudes in the northern
hemisphere, storminess is more important. Here, the
North Atlantic Oscillation is the controlling factor.
Similar influences may occur in western North
America due to changes in sea surface temperature in
the north Pacific.
The dominant factor controlling air movement across
the surface of the Earth is the movement of cold polar
air in the form of mobile polar highs from the poles
towards the equator. This drives global air circulation
and satisfies the requirement in the atmosphere to
balance the inequality in heating and cooling between
the equator and poles, respectively. The concept of
mobile polar highs implies that the climate of high
latitudes is the key to world climate and global climate
change. Superimposed upon this meridional exchange
are zonal processes controlled by ocean-atmosphere
interactions. Chief amongst these is the Southern
Oscillation. While droughts and floods have plagued
people throughout recorded history, and are probably
responsible for the greatest loss of life of any natural
 
 
Search WWH ::




Custom Search