Previous studies on the modification of
precipitation trends by quantile mapping have focused on mean quantities, with less attention paid to extremes.
Not exact matches
The methodology developed in Lovejoy's two recent papers could also be used
by researchers to help analyze
precipitation trends and regional climate variability and to develop new stochastic methods of climate forecasting, he adds.
There were no significant
trends in mean annual total
precipitation or total
precipitation affected area but we did observe a significant increase in mean annual rain - free days, where the mean number of dry days increased
by 1.31 days per decade and the global area affected
by anomalously dry years significantly increased
by 1.6 % per decade.
To assess Montana's historical climate, we evaluated temperature and
precipitation trends since the mid-20th century
by using standard statistical methods to analyze records of temperature and
precipitation.
> GHCN - Monthly is used operationally
by NCDC to monitor long - term
trends in temperature and
precipitation....
I have read
precipitation studies were more difficult due to sparse data, and it seems we would have seen
precipitation trend graphs a lot more often
by now if it was straight forward.
The aspect of the paper that has attracted the most attention is the claim that the retreat of the Kilimanjaro summit glaciers can be explained
by precipitation reduction, without any compelling need to invoke a warming
trend in local air temperature.
We do know that there are
trends in temperature extremes and
precipitation extremes (which are backed solidly
by physics in a warming climate), but for the other metrics we don't really see
trends at all.
At the tail end of the full paper, capping a paragraph about a weak spot in the analysis — that the observed
trend in extreme
precipitation events exceeds what is produced
by various climate models — comes a sentence about uncertainties:
As you can see, the variability around the
trend is largely explained
by temperature and
precipitation, while there is (near) zero influence on the
trend itself...
The atmospheric warming is the factor that can best explain this consistency, up to ~ 0.7 °C since 1950 and more marked since 1976, while the
trend in
precipitation is much less homogeneous over this area and is affected
by a significant decadal variability.
As researchers documented in this graph, the region had experienced increasing
precipitation during the Little Ice Age, followed
by a sharp drying
trend that began in the late 1700s, which triggered Kilimanjaro's retreat long before CO2 ever reached significant concentrations.
This
trend is driven
by daily highs and lows, availability of water and heavy
precipitation in a single day.
The number of stations reflecting a locally significant increase in the proportion of total annual
precipitation occurring in the upper five percentiles of daily
precipitation totals outweighs the number of stations with significantly decreasing
trends by more than 3 to 1 (Figure 2.36 c).
Note that the sign of
precipitation trends in areas most directly impacted
by the NAO such as southern Europe and the west coasts of Norway, the U.K. and Iceland, remains uncertain even for the next 50 years (Fig. 10d) consistent with the results shown in Figs.
For instance: in support of «temperatures and causality» he cites a paper
by Zhang et al on «Detection of human influence on twentieth century
precipitation trends».
[ISPM 2.2 a] This is followed
by a few examples of inconsistent regional
trends, as well as a statement concerning a lack of
trend in overall total
precipitation.
Puma and his coauthor, Benjamin Cook, a climatologist at Goddard and Columbia's Lamont - Doherty Earth Observatory, are the first to look at the historic effects of mass watering on climate globally
by analyzing temperature,
precipitation and irrigation
trends in a series of model simulations for the last century.
A study
by the Climate Service Center Germany (GERICS) discovered, according to Phys.org, that «
precipitation in Germany has increased
by 11 percent since 1881 — and according to the forecasts, this
trend is set to continue.
Singh and her Lamont colleagues research climate change impacts on weather patterns
by analyzing weather
trends in daily temperatures,
precipitation, and atmospheric patterns that have occurred during the past 40 years, in the post-satellite era.
«The recent
trends in winter
precipitation have been accompanied
by respective
trends in sunshine (significant increase in all subregions of 17 to 29 %)»
We find that the reported discrepancy can be traced to two main issues: (1) unforced internal climate variability strongly affects local wetness and dryness
trends and can obscure underlying agreement with WWDD, and (2) dry land regions are not constrained to become drier
by enhanced moisture divergence since evaporation can not exceed
precipitation over multiannual time scales.
A 2015 study found that warm conditions induced
by human - caused global warming have already increased the risk of severe drought in California, even in the absence of
trends in
precipitation.
«Our analysis is the first to bridge these gaps for a large range of impacts,
by assessing the role of human - related emissions in each impact individually, including impacts related to
trends in
precipitation and sea ice.»
b
Trends surface temperature from the GOGA CAM3 simulations (background colorscale; air temperature over sea ice and SST elsewhere) along with the Z850
trend produced
by the model simulations (black contours; negative dashed and positive solid; interval of 3 m / decade) and the simulated convective
precipitation trends (positive green contours, negative red contours, contoured at − 0.7, − 0.3, − 0.1, 0.1, 0.3, and 0.7 mm / day / decade, shown only for 45 ° S — 45 ° N. (c) As in (b) but for the TOGA CAM3 simulations.
Indeed, our results show that even in the absence of
trends in mean
precipitation — or
trends in the occurrence of extremely low -
precipitation events — the risk of severe drought in California has already increased due to extremely warm conditions induced
by anthropogenic global warming.
Scientists also factored long - term, climate change
trends into the three - month seasonal outlook
by looking at the last 10 to 15 years of temperature and
precipitation across the country.
The increasing humidity
trend below the troposphere might be compensated
by increase in convection and
precipitation.