SOLAR VARIABILITY: climatic change resulting from changes in the amount of solar energy reaching the upper atmosphere.

CHRONOLOGICAL SCALE
109 106 103 102 10 YR
    GEOLOGIC 1. 2. 2. 3. 3. 3. 3.
GEOGRAPHICAL SCALE
  Local  Regional  Global 
    GEOLOGIC     1. 2. 3.
The sun is the ultimate source of nearly all of the energy on earth. Approximately (2 cal cm-2 min-1) reach the top of the atmosphere. Changed by

1. SOLAR EVOLUTION

PARADOX: 4.5 billion years ago sun was ca. 8% smaller and ca. 3 % less luminous so solar constant was ca. 25 % less. As sun converts Hydrogen to Helium, the luminosity will continue to increase over next 4 by (Walter & Barry, 1991)



2. GLACIAL EPISODES (250 my cycle)

  • 1947 Umbgrove noted: Glacial ages occur on ca. 200 my cycle
  • Dilke and Gough (1972) propose that mixing in the sun's core produces periodic (ca. 109 yr) fluctuations in solar luminosity
  • STIENER - GRILLMAIR (1973) suggest that 250 my cycle in solar variability caused by the sun's orbit around the galaxy.
    • 7 of the 12 periods during the last 4.5 by when sun farthest from center of galaxy, have "documented" glaciations
    • 5 "missing" glacial episodes explained of lack of suitable geographical distribution of continents
    • mechanisms: when the earth is farthest "out"
      • lower gravity force = cooler sun due to slower circulation within sun
      • slower orbital velocity = sun accretes less Hydrogen, less fuel
  • Interstellar Dust?
Stiener Grillmair 73

3. SUNSPOTS AND SOLAR ACTIVITY

Historical Record
cycles
    R = k(10g+s)
    R is the Wolf sunspot number
    g is the number of sunspot groups on the solar disk
    s is the total number of individual spots in all groups
    k is a variable scaling factor (usually <1)
Cosmogenic Isotopes

Causes of 14C/12C ratio Fluctuations




Climate Correlations: COLD CLIMATE, SUNSPOT MINIMA, AND 14C ANOMALIES

Historic

Science NASA (cycle 22)

Little Ice Age


Medieval Warm Period

Wet MWP in the Southwest (Davis, 1994)
    Dry MWP Europe


Dry MWP in the Sierra Nevada, high lake-levels during positive 14C anomalies
SUNSPOT MINIMA PROXY RECORD LAKE HIGH STAND
Name Name Age 14C Age 10Be Jura Alps, Fr Mono L., CA
Dalton   1825 AD 1825 AD    
Maunder Maunder 1710 AD 1710 AD   Clover Ranch
Sporer Sporer 1550 AD 1510 AD   Danberg Beach
      AD 1450   10-ml road lowstand
Wolf Yuan 1330 AD 1290 AD   Rush Delta
      AD 1350   Simnis Ranch lowstand
Medieval Song 1050 AD 1010 AD   Post Office
      AD 1100   Lee Vining lowstand
Roman IV Medieval 690 AD 670 AD P.Maclu 2  
Roman III Wei 450 AD 430 AD    
      AD 300   Marina Lowstand
Roman II   270 AD 210 AD    
Roman I   90 AD 110 AD P.Maclu 1  
Greek   330 BC 290 BC Bourget  
Homeric   750 BC 770 BC Bourget  
Egyptian   1370 BC 1370 BC Pluvis  
Silver Lake   1870 BC 1910 BC   Dechambeau R.
Noachan   2850 BC 2870 BC    
Sumerian II   3290 BC 3490 BC Chalain  
Sumerian I   3570 BC 3690 BC    
Jerico   5190 BC 5030 BC Cern  
Sahelan   5950 BC 6230 BC    
Eddy, 1977;
Davis, 1992
Youji, 1983     Magny, 1993 Stine, 1990;
Stine, 1994


Correlation of solar luminosity and temperature over the last 1000 years

Modeling

SUNSPOT "MINIMA" - 14C ANOMALIES

Damon AD 1880-1930 Global Temp 0.5 oC lower (Jones, 1988)

L
I
A
5

Dalton AD 1795-1825 "Year Without Summer" 1813
Maunder AD 1650-1710 Little Ice Age, Global Temp 1-2 oC lower
Sporer AD 1420-1540 Second Little Ice Age event
Wolf AD 1280-1340 The Great Drought
Greek 330 BC
Homeric 750 BC
Egyptian 1370 BC
Silver Lake 1870 BC
Noachan 2850 BC
The Greek and Homeric events together have been called the "Hallstat Period"
- a precurson or the Little Ice Age. REF
All names informal, those in bold are in common usage.


CYCLICITY & PREDICTABILITY

Because 14C cycles quasi periodic, Damon and Sonett (1989) predict future climate

Cycle
length
Cycle
name
Last positive
14C anomaly
Next
"warming"
2241 Landscheidt AD 1400 (cool) AD 2520
512 --?-- not used *
232 --?-- AD 1922 (cool) AD 2038
208 Suess AD 1898 (cool) AD 2002
88 Gleisberg AD 1986 (cool) AD 2030
22 Schwabe
11 Hale

* REFERENCES TO 512 YEAR CYCLE
  1. Chapman, M.R. and Shackleton, N.J. (2000). Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene. Holocene. 2000; 10(3): 287-291.

  2. (Eglinton et al., 1992 Nature 356: 423-426. ) NW Africa ODP core had strong 590 and 550 yr cycles from Termination IV.

  3. (Pederson, 2000 GSA Bulletin 112: 147-158.) SE Utah Lake Canyon & Black Mesa 500-550 yr wet-dry cycles late Holocene, also tree rings.

  4. Sarnthein, M., van Kreveld, S., Erlenkeuser, H., Grootes, P.M., Kucera, M., Pflaumann, U., and M. Schulz. Centennial-to-millennial-scale periodicities of Holocene climate and sediment injections off the western Barents shelf, 75°N. (Boreas, in press).

  5. Schulz, M. & Paul, A. 2002: Holocene climate variability on centennial-to- millennial time scales: 1. Climate records from the North-Atlantic realm. In Wefer, G., Berger, W. H., Behre, K.-E. & Jansen, E. (eds.): Climate development and history of the North Atlantic Realm, 41-54. Springer Verlag, Berlin. (Available from first authors' web site: http://www.palmod.uni-bremen.de/~mschulz/)

  6. (Sonett & Suess, 1984 Nature 307: 141-143.) They mention a "very strong" 500 year signal in limber pine from southern CA.

  7. Stager et al., 1997. Quat Res. 47:81-89) 510 year cycle from Lake Victoria, East Africa, diatom record. My newest core from the lake also show it.

  8. (Stuiver et al., 1995 Quat. Res. 44:341-354.) Got near 530 yr cycle in GISP2 ice core, postulated solar

  9. (Stuiver & Brauzanias, 1993 Nature 338:405-408) Cited in Mayewski et al JGR 1997.......Early Holocene had ca. 512 yr cycle maybe related to marine circulation. It's also in GISP2

  10. (von Rad et al., 1999 Quat. Res. 51: 39-53.): Arabian Sea OMZ core had significant 500 yr cycle

  11. Yu and Ito. Possible solar forcing of century-scale drought frequency in the northern Great Plains. Geology 27: 263-266.
PALEOCLIMATE LISTSERV Friday, February 28, 2003 11:30 AM, Tuesday, March 04, 2003 8:31 AM, Dr. Sushma Prasad, JAY C STAGER [stagerj@paulsmiths.edu]



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