There are other aspects to changes in precipitation that are noted, for instance, changes to large-scale atmospheric wind patterns push wet and dry regions to different parts of the planet.
All trend rates are expressed as a change per decade (except where otherwise noted), and precipitation trends were calculated as the percent change from the average of the entire analysis period 1951 2002.
Although it has to be noted that precipitation changes are harder to predict.
They had noted that precipitation can occur even at severely cold temperatures.
Exceptionally high amounts of precipitation (156.6 mm) were noted in October 1999.
Such precipitation processes have been noted previously to lead to a decrease in reaction rates and a loss in Cr VI) removal capacity in ZVI permeable barriers [78,79].
To investigate the interaction with LPS, we titrated in aliquots of LPS to a final probe (1)/LPS w/w ratio of 0.75:1.0 without precipitation (vide supra) and noted several small amide shifts in fast exchange for Dab1, Thr2, Dab9, Thr12, and Leu7.
The main reason for this is that a small number of wet days does not allow a good estimation of the conditional distribution of precipitation amounts; we note that the average probability of a dry day in this region is 86%.
The altitude effect was noted both in precipitation and in dripwater isotopic composition, but with notably different Δδ18O/100 m gradients (−0.33‰ and −0.11‰, respectively).
The evolution of the substorm concept to include phenomena outside the ionosphere began with a paper by Jelly and Brice (1967) which noted that "…auroral precipitation is not a spatially isolated phenomenon, but is intimately connected with large-scale processes that occupy a substantial part of the magnetosphere".
It may be noted that protein precipitation using a 1 1 solvent-to-serum ratio retained a high level of residual proteins compared with the 2 1 ratio for both methanol and acetonitrile, and hence, the 1 1 ratio was not considered for further quantitative evaluation (see SI Figures S2 and S3).
