Climatic Change Volume 109, Issue 3 - 4, pp 287 - 317.
Not exact matches
I would also like to add that the paper: Glacial geological evidence for the medieval warm period (
Climatic Change,
Volume 26, Numbers 2 - 3, pp. 143 - 169, March 1994)- Jean M. Grove, Roy Switsur is available as PDF on Google Books.
Climatic Change, June 2006,
Volume 76, Issue 3 - 4, pp 443 - 457, 10 Jun 2006 The Possible
Climatic Impact in China of Iceland's Eldgjá Eruption Inferred from Historical Sources Jie Fei, Jie Zhou
«
Climatic Change 100th
Volume: Be Careful What You Wish For!
They concluded that with a bit of help from
changes in solar output and natural
climatic cycles such as the El Nino Southern Oscillation (ENSO), the growth in the
volume of aerosols being pumped up power station chimneys was probably enough to block the warming effect of rising greenhouse gas emissions over the period 1998 - 2008.
Although the surface of the Greenland ice sheet can react rapidly to day - to - day weather
changes, the melting of the
volume of ice below is actually an inert process — driven by
climatic changes instead of single meteorological events.
Sources, if required, for para beginning «The peer - reviewed literature»: Deacon, E.L. 1952,
Climatic Change in Australia since 1880, Australian Journal of Physics,
Volume 6, Pages 209 - 218, see especially Figure 1 showing the ten - year running averages of mean summer maximum temperature for Bourke, Alice Springs Narrabri and Hay)
I would also like to add that the paper: Glacial geological evidence for the medieval warm period (
Climatic Change,
Volume 26, Numbers 2 - 3, pp. 143 - 169, March 1994)- Jean M. Grove, Roy Switsur is available as PDF on Google Books.
I've always thought that it was Linda Nash and Peter Gleick, back in 1991, who first predicted it (Sensitivity of streamflow in the Colorado Basin to
climatic changes, Journal of Hydrology
Volume 125, Issues 3 - 4, July 1991, Pages 221 - 241).
The temperature record is less complete for the deep ocean, and its massive
volume and separation from the surface subdues its response to
climatic changes.