titolar  
     
     
  WHAT HAPPENS WITH CLIMATE CHANGE?
- The natural causes of climate variation (including abrupt change)
- The effects of human activity on climate
- The Global Change
- Selected references
 
  PROJECT DESCRIPTION
 
  SCIENTIFIC RESULTS
 
  THE PROJECT
PARTNERS
 
  FOR PROJECT PARTICIPANTS
 
  ADMINISTRATIVE
MATTERS
   
 

SELECTED REFERENCES

 
 
Bond, G., Showers, W., Elliot, M., Evans, M. N., Lotti, R., Hajdas, I., Bonani, G., and Johnson, S. (1999). The North Atlantic’s 1-2 kyr climate rhythm: Relation to Heinrich Events, Dansgaard/Oeschger and the Little Ice Age. In “Mechanisms of global climate change at millennial time scales.” (P. U. Clark, R. S. Webb, and L. D. Keigwin, Eds.), pp. 35-58. Geophysical Monograph. American Geophysical Union, Washington.
Bryden, H. L., Longworth, H. R. and Cunningham, S. A. (2005) Slowing of the Atlantic meridional overturning circulation at 258N.  Nature 438, 655–657.
Cacho, I., Grimalt, J.O., Pelejero, C., Canals, M., Sierro, F.J., Flores, J.A. and Shackleton, N. (1999) Dansgaard-Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures. Paleoceanography 14, 698-705.
Cacho, I., Grimalt, J. O., Canals, M., Sbaffi, L., Shackleton, N. J., Schönfeld, J., and Zahn, R. (2001). Variability of the western Mediterranean Sea surface temperatures during the last 25,000 years and its connection with the northern hemisphere climatic changes. Paleoceanography 16, 40-52.
deMenocal, P., Ortiz, J., Guilderson, T. P., and Sarnthein, M. (2000). Coherent high- and low- climate variability during the Holocene warm period. Science 288, 2198-2202.
Frigola, J., Moreno, A., Cacho, I., Canals, M., Sierro, F.J., Flores, J.A., Grimalt, J.O., Hodell, D.A. and Curtis, J.H. (2007). A deep water sediment record of Holocene climate variability in the Western Mediterranean region. Paleoceanography 22, PA2209, doi: 10.1029/2006PA001307.
Grimalt, J.O. and Martrat, B. (2008) The bipolar seesaw on the Iberian Margin stretching over the past 420,000 years. Past Global Changes 16, 25-27.
Hansen, B., Turrell, W.R.  and Østerhus, S.  (2001) Decreasing overflow from the Nordic seas into the Atlantic Ocean through the Faroe Bank channel since 1950. Nature 411, 927-930.
Kearney, M.S., Rogers, A.S., Townshend, J.R,G., Rizzo, E., Stutzer, D., Stevenson, J.C, and Sundborg, K. (2002) Landsat Imagery Shows Decline of Coastal Marshes in Chesapeake and Delaware Bays, Eos Transactions 83, 173-175.
Mann, M.E., Bradley, R.S. and Hughes, M.K. (1998) Global-scale temperature patterns and climate forcing over the past six centuries Nature 392, 779 - 787.
Marchal, O., Cacho, I., Stocker, T. F., Grimalt, J. O., Calvo, E., Martrat, B., Shackleton, N. J., Vautravers, M., Cortijo, E., van Kreveld, S. A., Andersson, C., Koç, N., Chapman, M. R., Sbaffi, L., Duplessy, J. C., Sarnthein, M., Turon, J. L., Duprat, J., and Jansen, E. (2002). Apparent long-term cooling of the sea surface in the Northeast Atlantic and Mediterranean during the Holocene. Quaternary Science Reviews 21, 455-483.
Martrat, B., Grimalt, J.O., Lopez-Martinez, C., Cacho, I., Sierro, F.J., Flores, J.A., Zahn, R., Canals, M., Curtis, J.H. and Hodell, D.A. (2004) Abrupt temperature changes in the western Mediterranean over the past 250,000 years. Science 306, 1762-1765.
B. Martrat, J.O. Grimalt, N.J. Shackleton, L. de Abreu, M.A. Hutterli and T.F. Stocker (2007) Four climate cycles of recurring deep and surface water destabilizations on the Iberian Margin. Science 317, 502-507.
NOAA, 2007. http://www.ncdc.noaa.gov/oa/climate/research/2005/ann/global.html
Petit, J. R., Jouzel, J., Raynaud, D., Barkov, N. I., Barnola, J. M., Basile, I., Bender, M., Chappellaz, J., Davis, M., Delaygue, G., Delmotte, M., Kotlyakov, V. M., Legrand, M., Lipenkov, V. Y., Lorius, C., Pépin, L., Ritz, C., Saltzman, E., and Stievenard, M. (1999). Climate and atmospheric history of the past 420,000 years from the Vostok ice cores, Antartica. Nature 399, 429-436.
Pla S, Catalan J (2005) Chrysophyte cysts from lake sediments reveal the submillennial winter/spring climate variability in the northwestern Mediterranean region throughout the Holocene. Clymate Dynamics, 24: 263-27.
Sanchez-Goñi, M.F., Cacho, I., Turon, J.-L., Guiot, J., Sierro, F.J., Peypouquet, J.-P., Grimalt, J.O. and Schackleton, N.J. (2002) Synchroneity between marine and terrestrial responses to millennial scale climatic variability during the last glacial period in the Mediterranean region. Climate Dynamics 19, 95-105.

Siegenthaler, U., Stocker, T. F., Monnin, E., Luthi, D., Schwander, J., Stauffer, B., Raynaud, D., Barnola, J.-M., Fischer, H., Masson-Delmotte, V., and Jouzel, J. (2005). Stable Carbon Cycle-Climate Relationship During the Late Pleistocene 10.1126/science.1120130. Science 310, 1313-1317.
Stocker T.F., A. Schmittner (1997) Rate of global warming determines the stability of the ocean-atmosphere system. Nature 388, 862-865.