Moreover, local
heavy precipitation trends may not accurately reflect changing patterns happening at a larger, regional level.
The flooding continued
the heavy precipitation trend of 2010, which was the wettest year on record.
Not exact matches
With flooding in parts of the Mississippi Valley and a strong Pacific storm coming into the Northwest, we examined the
trend in the number of days each year with
heavy precipitation at 244 individual sites in the U.S..
However, combined measuring stations around the world suggest there has been a global
trend towards more frequent and intense hot extremes since the 1950s, as well as more
heavy precipitation events.
These variability
trends indicate that the frequency of extremes (more drought events and more
heavy precipitation events) has increased whereas the mean has remained approximately the same.
This apparent inconsistency says little about the overall
trend in the
heaviest precipitation events, but a lot about the weaknesses of single - point measurements for detecting
trends in extreme
precipitation.
As a consequence, even in regions or states where there is a strong increasing
trend in
heavy precipitation, the
trend at an individual
precipitation gauge that represents the official total for a city may be equivocal, flat, or even down.
Percent changes in the amount of
precipitation falling in very
heavy events (defined as the
heaviest 1 percent of events) from 1958 to 2012 show a clear national
trend toward a greater amount of
precipitation being concentrated in very
heavy events.
Of course, many individual locations show strong increasing
trends in the
heaviest precipitation events.
Snowfall varies across the region, comprising less than 10 % of total
precipitation in the south, to more than half in the north, with as much as two inches of water available in the snowpack at the beginning of spring melt in the northern reaches of the river basins.81 When this amount of snowmelt is combined with
heavy rainfall, the resulting flooding can be widespread and catastrophic (see «Cedar Rapids: A Tale of Vulnerability and Response»).82 Historical observations indicate declines in the frequency of high magnitude snowfall years over much of the Midwest, 83 but an increase in lake effect snowfall.61 These divergent
trends and their inverse relationships with air temperatures make overall projections of regional impacts of the associated snowmelt extremely difficult.
Observed U.S.
trends in
heavy precipitation (Kunkel et al. 2013)
Projections of future climate over the U.S. suggest that the recent
trend towards increased
heavy precipitation events will continue.
For the entire Northern Hemisphere, there is evidence of an increase in both storm frequency and intensity during the cold season since 1950,1 with storm tracks having shifted slightly towards the poles.2, 3 Extremely
heavy snowstorms increased in number during the last century in northern and eastern parts of the United States, but have been less frequent since 2000.11,15 Total seasonal snowfall has generally decreased in southern and some western areas, 16 increased in the northern Great Plains and Great Lakes region, 16,17 and not changed in other areas, such as the Sierra Nevada, although snow is melting earlier in the year and more
precipitation is falling as rain versus snow.18 Very snowy winters have generally been decreasing in frequency in most regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19
Heavier - than - normal snowfalls recently observed in the Midwest and Northeast U.S. in some years, with little snow in other years, are consistent with indications of increased blocking (a large scale pressure pattern with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about
trends in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of
trends in blocking remains an active research area.
This
trend is driven by daily highs and lows, availability of water and
heavy precipitation in a single day.
While there has been a recent increase in the number of landfalling US hurricanes, the increase in tropical cyclone - associated
heavy events is much higher than would be expected from the pre-1994 association between the two, indicating that the upward
trend in
heavy precipitation events is due to an increase in the number of
heavy precipitation events per system.
The widespread
trend of increasing
heavy downpours is expected to continue, with
precipitation becoming less frequent but more intense.13, 14,15,16 The patterns of the projected changes of
precipitation do not contain the spatial details that characterize observed
precipitation, especially in mountainous terrain, because the projections are averages from multiple models and because the effective resolution of global climate models is roughly 100 - 200 miles.
There is a clear national
trend toward a greater amount of
precipitation being concentrated in very
heavy events, particularly in the Northeast and Midwest.
Many climate studies assess
trends and projections in
heavy precipitation events using
precipitation percentile (or quantile) indices.
... «stations experiencing low, moderate and
heavy annual
precipitation did not show very different
precipitation trends,»... «deserts / jungles are neither expanding nor shrinking due to changes in
precipitation patterns.»