Day 47: Impacts of the Western Ridge
Last night I mentioned the persistent upper-level high (referred to as an upper-level ridge) that was redeveloping across the western United States. In that post I mentioned that one result of this upper-level high would be warmer than normal temperatures across portions of the west. Another impact is a lack of precipitation.
The image above displays the current “Drought Monitor” for the United States, including Alaska and Hawaii, produced by the National Drought Mitigation Center. Areas shaded in yellow (bad) to red (worst) indicate areas where there is an ongoing drought. Notice how for most of the country, little to no drought is found – including places in southern Texas that were experiencing an extreme drought just last summer. One place where drought is a developing concern is the western United States, which has been under the west coast ridge for a good portion of the winter. This west coast ridge extends all the way up into Alaska, and the beginnings of a drought are observed there as well.
Another place that is experiencing a drought is Hawaii. This is the result of a different upper-level high (also the result of an El Nino winter). This upper-level high over Hawaii made my Snow Shot of America project “interesting” as the lack of Hawaiian precipitation has resulted in less snow on the peaks than is normally expected.



