An analytical solution for A should allow us to predict experimental
outcomes, should let us compare survival strategies, and should reveal the
general features of phase variation.
As Habermas has argued, dialogue should allow participants at least
the possibility of reaching 'more truthful interpretations of their own
particular needs as well as especially of those which are common and capable
of consensus.'
The thickness of the sediment layers (0.2-0.4 m), their high debris
concentrations and massive (as opposed to laminated) structure allow us to
dismiss regelation across basal obstacles as a possible debris entrainment
mechanism at Storglaciaren.