The National Snow and Ice Data Center (NSIDC) serves as the national information center that supports research in glaciers and freezing weather phenomena. The NSIDC archives snow and ice data and maintains information about everything from avalanches to icebergs. The NSIDC web site contains a fascinating list of Quick Facts about snow that are sure to be of interest to anyone experiencing winter weather.
La Niña
La Niña refers to a period when ocean temperatures across the central and eastern tropical Pacific Ocean are cooler than normal. The cooling of the ocean waters leads to changes in the patterns of tropical rainfall from Indonesia to South America, a distance of more than one-half the circumference of the Earth, which significantly affects the strength and location of the atmospheric jet stream over the eastern North Pacific and North America. These changes in the jet stream alter U.S. weather patterns.
La Niña patterns can be categorized according to the combined strength, location and coverage of the cold ocean waters. Moderate-to-strong La Niña systems impact the weather patterns in a similar manner, and thus this distinction is thought by many to have little meaning. The weather patterns with a weak La Niña tend to be somewhere in between those of a stronger episode and those of near-neutral conditions.
North Atlantic Oscillation
Global-scale circulation patterns are a natural part of our climate and occur independent of the La Niña influence. The North Atlantic Oscillation (NAO) is one such wild card. The NAO reflects large-scale changes in the portion of the jet stream which extends from the eastern United States to Europe. The NAO exhibits an enormous degree of variability because it can persist for years in a particular state and then transition to a completely different phase the next winter. It can also vary substantially within a given year. This variability, as well as the El Niño-La Niña cycle, are major contributors to the differences in weather patterns from one winter to the next and to the variability in weather within a given winter season. Scientists have not yet identified a clear climate signal that will give us a meaningful hint as to the state of the NAO during an upcoming winter.
The NAO has affected the La Niña signal in the past. In the eastern United States, the cold and snowy 1995/96 winter and the very mild 1998/99 winter were both La Niña winters. However, the opposite phases of the NAO during these two winters contributed significantly to the difference between them. Therefore, exercise caution when comparing one La Niña to the next.