Bracken C., B. Rajagopalan, L. Cheng, W. Kleiber and S. Gangopadhyay (August 2016): Spatial Bayesian hierarchical modeling of
precipitation extremes over a large domain.
In addition, climate change is very likely to lead to more frequent extreme heat events and daily
precipitation extremes over most areas of North America, more frequent low snow years, and shifts towards earlier snowmelt runoff over much of the western US and Canada (high confidence).
O'Gorman, P. A., and T. Schneider, 2009: Scaling of
precipitation extremes over a wide range of climates simulated with an idealized GCM.
«We show that at the present - day warming of 0.85 °C about 18 % of the moderate daily
precipitation extremes over land are attributable to the observed temperature increase since pre-industrial times, which in turn primarily results from human influence,» the research team said.
Not exact matches
«If we look at
precipitation events
over the long term, there is an increase in frequency of
extremes.
Based on
over a decade of asthma hospitalization data (115,923 cases from 2000 - 2012), researchers observed higher risk of asthma hospitalization after
extreme heat or
extreme precipitation events.
Staying on the Southern Hemisphere, a research team led by Sue Rosier, looked at
extreme precipitation over the North Island of New Zealand that led to severe flooding in July 2014.
The
Extremes Grand Challenge is organised around four
over arching themes (Document, Understand, Simulate, Attribute) with a main focus on four core events (Heavy
Precipitation, Heatwave, Drought, Storm).
I understand this to mean that
over time, there is a tendency to move upwards (to the right) along the cumulative probability curve, let's say, for annual
extreme 1 - day
precipitation.
My experience with
extremes and detection and attribution of an anthropogenic signal in those is that only by averaging the behavior of
extremes (both temperature
extremes and
precipitation extremes)
over large geographical areas (continental or barely sub-continental) we have been able to see something outside of natural variability.
Second Assessment of Climate Change for the Baltic Sea Basin https://books.google.com/books?isbn=3319160060 The BACC II Author Team averaged frequency of
extreme 1 - day
precipitation totals above 15 mm and a... 4.6 Cloudiness and Solar Radiation 4.6.1 Cloudiness Records of cloudiness and solar... There is a trend of decreasing cloud cover
over the Baltic Sea basin......
These results are based on a comparison of observed and multi-model simulated changes in
extreme precipitation over the latter half of the twentieth century analyzed with an optimal fingerprinting technique.
I posted a quick riff overnight on new research, published in Nature, that links human - driven global warming and rising instances of
extreme precipitation in observed parts of the Northern Hemisphere
over the last half of the 20th century.
The U.S. Climate
Extremes Index (USCEI), an index that tracks the highest and lowest 10 percent of extremes in temperature, precipitation, drought and tropical cyclones across the contiguous U.S., was a record - large 44 percent during the January - June period, over twice the averag
Extremes Index (USCEI), an index that tracks the highest and lowest 10 percent of
extremes in temperature, precipitation, drought and tropical cyclones across the contiguous U.S., was a record - large 44 percent during the January - June period, over twice the averag
extremes in temperature,
precipitation, drought and tropical cyclones across the contiguous U.S., was a record - large 44 percent during the January - June period,
over twice the average value.
Nearly all studies to date published in the peer - reviewed literature agree that
extreme precipitation event number and intensity have risen, when averaged
over the United States.
Maine could also see two to three times more
extreme precipitation events, defined as four inches
over 48 hours, said Wake.
There is a minimum model resolution that is needed to capture weather phenomena generating
precipitation extremes, for example for simulating tropical cyclones or
precipitation enhancement
over mountains.
«Lehmann et al. (2015) also found large — scale increasing patterns in
extreme precipitation, with 12 % more record - breaking rainfall events
over 1981 — 2010.
The US CLIVAR
Extremes Working Group was formed to evaluate whether current climate models produce extremes for the right reasons and whether they can be used for predicting and projecting short - term extremes in temperature and precipitation over North
Extremes Working Group was formed to evaluate whether current climate models produce
extremes for the right reasons and whether they can be used for predicting and projecting short - term extremes in temperature and precipitation over North
extremes for the right reasons and whether they can be used for predicting and projecting short - term
extremes in temperature and precipitation over North
extremes in temperature and
precipitation over North America.
On
extreme precipitation events
over mid-latitude landmass and wet tropical regions becoming more intense and frequent, the CLAs clarified that the assessment was based on more than the RCPs, and that the conclusion was generally true for all these regions.
Over the longer term, this kind of weather isn't totally unexpected —
extreme swings in
precipitation are becoming the new normal.
* I was just recently pointed at a study by Cretat et al (http://link.springer.com/article/10.1007/s00382-013-1796-7) demonstrating the added skill of RCMs
over GCMs to capture the characteristics of
extreme precipitation events
over Africa
The report, written by 220 experts from 62 countries, finds that climate change has already contributed to changes in
extreme events — such as heat waves, high temperatures, and heavy
precipitation — in many regions
over the past 50 years.
Average
precipitation is changing in many regions with both increases and decreases and there is a general tendency for increases in
extreme precipitation observed
over land areas.
Hagos, S. M., et al., 2016: A projection of changes in landfalling atmospheric river frequency and
extreme precipitation over western North America from the Large Ensemble CESM simulations.
One of the major findings is an increase in key types of
extreme weather events, especially in heat waves and large
precipitation events, in the U.S. and around the world
over the last 50 years.
This report discusses our current understanding of the mechanisms that link declines in Arctic sea ice cover, loss of high - latitude snow cover, changes in Arctic - region energy fluxes, atmospheric circulation patterns, and the occurrence of
extreme weather events; possible implications of more severe loss of summer Arctic sea ice upon weather patterns at lower latitudes; major gaps in our understanding, and observational and / or modeling efforts that are needed to fill those gaps; and current opportunities and limitations for using Arctic sea ice predictions to assess the risk of temperature /
precipitation anomalies and
extreme weather events
over northern continents.
Winter
precipitation (mean and
extreme) variability and trends along the south coast and interior of Alaska appear to be closely related to variations in the PNA pattern
over this timeframe, while El Nino / Southern Oscillation (ENSO) influences, through the Nino3 index, appear to be significant along the south coast alone.
The projections also indicate an increase in the basin - averaged
precipitation and an increase in the frequency of
extreme precipitation events
over the region as a whole.
Zilli M. T., L. M. V. Carvalho, B. Liebmann and M. A. S. Dias (April 2017): A comprehensive analysis of trends in
extreme precipitation over southeastern coast of Brazil.
Wang, J. & Zhang, X. Downscaling and projection of winter
extreme daily
precipitation over North America.
Although the global models have improved
over time (Chapter 8), they still have limitations that affect the simulation of
extreme events in terms of spatial resolution, simulation errors, and parametrizations that must represent processes that can not yet be included explicitly in the models, particularly dealing with clouds and
precipitation (Meehl et al., 2000d).
In general, the majority of all
precipitation occurs as isolated 1 - day events, while most
extreme precipitation occurs
over a period of several hours embedded within 2 - 5 day events.
Over 75 % of the Northeast short - term
extreme precipitation is related to extratropical storms moving through or near the region, except during September, when more than 50 % of
extreme precipitation is related to tropical storm activity.
The culprit behind much of the
extreme heat in each case has been large, strong, and persistent areas of high pressure, which have set up shop
over these high latitude locations, keeping cooler weather and
precipitation at bay.
Here is an excerpt of the research paper, «When It Rains It Pours», from Environment America, showing a statistically significant spike in flash flooding and other
extreme precipitation events since 1948: «Weather records show that storms with
extreme precipitation have become more frequent
over the last 60 years.
An analysis of
extreme precipitation trends in Europe during the 20th century has identified a wetting trend
over central and western Europe from 1921 to 1999.
Many impacts of climate change will be realised as the result of a change in the frequency of occurrence of
extreme weather events such as windstorms, tornados, hail, heatwaves, gales, heavy
precipitation or
extreme temperatures
over a few hours to several days.