Holocene hydrological changes in south - western Mediterranean as recorded by lake - level fluctuations at Lago Preola, a coastal lake in southern Sicily, Italy, Magny et al, 06/2011; read more here.
Holocene hydrological changes in south - western Mediterranean as recorded by lake - level fluctuations at Lago Preola, a coastal lake in southern Sicily, Italy; Magny et al, 2011, see abstract here.
Oxygen - isotope (λ 18O) evidence of
Holocene hydrological changes at Signy Island, maritime Antarctica Noon, P.E., Leng, M.J. and Jones, V.J. 2003; The Holocene 13: 251 - 263
Not exact matches
Hydrological and Climatological
Changes in the Trondheimsfjord / Norway during the late
Holocene inferred from Benthic Stable Isotopes and Dinocyst Assemblages G. Milzer, J. Giraudeau, S. Schmidt, J. Faust, J. Knies, F. Eynaud, C. Rühlemann > Download
The end of the first half of the
Holocene — between about 5 and 4 ka — was punctuated by rapid events at various latitudes, such as an abrupt increase in NH sea ice cover (Jennings et al., 2001); a decrease in Greenland deuterium excess, reflecting a
change in the
hydrological cycle (Masson - Delmotte et al., 2005b); abrupt cooling events in European climate (Seppa and Birks, 2001; Lauritzen, 2003); widespread North American drought for centuries (Booth et al., 2005); and
changes in South American climate (Marchant and Hooghiemstra, 2004).
The temporal relationship between the Suess solar cycle and particularly significant 210 yr oscillations in the speleothem δ18O records therefore supports the notion that solar variability played a significant role in driving centennial - scale
changes in the
hydrological cycle in the subtropics during the
Holocene.