Tim Bardsley and Mark W. Williams
Institute of Arctic and Alpine Research and
Department of Geography, CB 450,
University of Colorado, Boulder, CO
Figure 5.
However, annual solid precipitation (October-May)
of 1514 mm measured at the saddle was 61% more than
the 938 mm measured at D1 and accounted for the
difference in annual precipitation amount at the two sites.
A paired t-test shows that precipitation amount
at the saddle was significantly greater than at D1
(p = 0.001, n = 9).