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Paleoclimatic records of the Great Plains, including The most severe sustained drought in the tree-ring <br /> the South Platte River Basin and the Arkansas River record for the Rio Grande Basin occurred in 1573- <br /> basin, indicate that widespread prolonged drought 1592. <br /> (3-10 years) equaled or surpassed the 1930's <br /> drought in intensity and duration in the late 1750s, <br /> early 1820s, and early 1860s. Major droughts that a ' <br /> likely exceeded twentieth century droughts occurred 1- - <br /> on the Great Plains in the second part of the 16th w 0 �i If. ��., 1 i! at, l,. 1. ,� �I <br /> century (possibly the periods 1539 to1564 and from ;, T 1i T <br /> 1587 to 1605) and the last quarter of the 13th a-1 <br /> century (possibly from1276 to1313). The evidence -2- `1573_15s2 - <br /> further suggests at least four periods of widespread <br /> multi-decadal drought occurred on the Great Plains 100 1000 1100 1200 1300 140Ye1500 1600 1700 1800 1900 <br /> between A. D. 1 and 1200 (roughly in the periods <br /> 250-300, 750-800, 940-990, and 1130-1180). <br /> Arkansas River Basin San Miguel-Dolores-San Juan River Basins <br /> Sufficient precipitation records are available from Sufficient precipitation records are available from <br /> 1891 in the lower Arkansas River Basin and from 1898. Recent droughts in the San Miguel-Dolores- <br /> 1880 in the upper basin. Recent droughts in the San Juan River Basins occurred in 1899-1905 <br /> lower Arkansas River Basin occurred in 1894-1898, (extreme), 1918-1919, 1931-1936, 1945-1947, <br /> 1911-1913, 1934-1941 (extreme), 1952-1957, 1964- 1951-1952, 1954-1957, 1976-1978, and 1989-1991. <br /> 1966, 1974-1977, and 1981-1982. Recent droughts The most sustained drought in the tree-ring record <br /> in the upper Arkansas River Basin occurred in for the San Miguel-Dolores-San Juan River Basins <br /> 1880-1881 (extreme), 1888-1894, 1907-1909, 1932- occurred in 1273-1289. Many archaeologists <br /> 1940, 1950-1956, 1963-1965, and 1975-1977. believe this period of severe sustained drought <br /> coincided with the abandonment of Mesa Verde by <br /> Tree-ring Record for Southeastern Colorado the Anasazi. Several shorter, but more severe <br /> (Point 60),1700-1979 droughts, were identified between AD 512 and <br /> 6.0 1673. <br /> O. 40 <br /> K <br /> l fl <br /> a <br /> i1IWI!IIWfI ! <br /> Mesa Ve rde Deocinade N oo1 (I�14 ao� <br /> al A.D.•196$AD. <br /> 2.7 a 11111111111111 Lillilthii n <br /> . <br /> a.o 't I <br /> a3 ra.rwr <br /> O. ,.. tza .1 ,, yf - if t Ii - <br /> li _ e 1i �t. F ! I 1,1 5 . ! - ~taar r <br /> ii r r <br /> s.o � <br /> I: <br /> ' L1 11 1. 11 ..1 _ <br /> a <br /> Rio Grande Basin 481 201 681 181 b1 981 1981 1181 1111 1351 1411 1601 1E11 1181 1881 1981 <br /> Tar <br /> Sufficient precipitation records in the Rio Grande °-'°~ °- 6ie ° <br /> Basin are available from 1897. Recent droughts in <br /> the Rio Grande Basin occurred in 1897, 1900-1906, <br /> 1923, 1939-1940, 1943-1947, 1950-1952 (extreme), <br /> 1955-1956, 1963-1964, 1972-1973, and 1996-1997. <br /> 4 <br />