It will depend on what is available at that time, quality checking and climate model constraints.We will involve several PMIP participants in the process, and you are all invited to comment on the proposition in the (at the bottom of this page).
https://en.wikipedia.org/wiki/Maunder_Minimum See: https://malagabay.wordpress.com/2017/04/06/deranged-dating-intcal13-and-the-heinsohn-horizon/ Although this deference to the glaciologists and their Beryllium-10 Ice Core Chronologies is very touching the independent observer should establish whether this deference is justified. The primary issue is that the rapid downward oscillations in the Beryllium-10 Chronology from the Dye-3 Ice Core don’t emulate the observed atmospheric Carbon-14 Decay Curve.
Atmospheric δ14C Record from Wellington Carbon Dioxide Information Analysis Center 10 variations As of 1998 the only long record available for 10Be is from Dye 3 1979.
The following plots were generated using the latest versions of the reconstructions available to the persons who made the plots and may be more up-to-date than the plots available in the sections below.
Please try to use the most recent plots when commenting the reconstructions!
It has become increasingly clear that these radiometric dating techniques agree with each other and as a whole, present a coherent picture in which the Earth was created a very long time ago.
Further evidence comes from the complete agreement between radiometric dates and other dating methods such as counting tree rings or glacier ice core layers.Fission products include radionuclides such as 14C and 10Be that settle on the Earth’s surface.Their concentration can be measured in ice cores, allowing a reconstruction of solar activity levels into the distant past.Several PMIP participants are in favour of using a new ice-sheet reconstruction that better matches the geomorphologic and glaciological constraints than ICE-5G used in PMIP2.We plan thus to have - a reference ice-sheet for the core simulations - alternatives for groups interested to run sensitivity experiment in order to discuss the sensitivity of the model results to the uncertainties in boundary conditions.Images, videos and audio are available under their respective licenses.