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Strong increase in convective precipitation in response to higher temperatures

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TLDR
In this paper, a combination of radar and rain gauge measurements over Germany with synoptic observations and temperature records reveals that convective precipitation, for example from thunderstorms, dominates events of extreme precipitation.
Abstract
The intensity of extreme precipitation rises faster than the rate of increase in the atmosphere’s water-holding capacity. A combination of radar and rain gauge measurements over Germany with synoptic observations and temperature records reveals that convective precipitation, for example from thunderstorms, dominates events of extreme precipitation.

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Future changes to the intensity and frequency of short‐duration extreme rainfall

TL;DR: In this paper, a review examines the evidence for sub-daily extreme rainfall intensification due to anthropogenic climate change and describes the current physical understanding of the association between sub-day extreme rainfall intensity and atmospheric temperature.
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Bias Correction of GCM Precipitation by Quantile Mapping: How Well Do Methods Preserve Changes in Quantiles and Extremes?

TL;DR: In this paper, the authors investigated the extent to which quantile mapping algorithms modify global climate model (GCM) trends in mean precipitation and precipitation extremes indices, and proposed a bias correction algorithm, quantile delta mapping (QDM), that explicitly preserves relative changes in precipitation quantiles.
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Heavier summer downpours with climate change revealed by weather forecast resolution model

TL;DR: This article used a high-resolution model, typically used for weather forecasting, to simulate hourly rainfall in the UK in the year 2100 and found that short-duration rainfall intensified in summer, increasing the risk of flash flooding.
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Precipitation Extremes Under Climate Change.

TL;DR: In this paper, the response of precipitation extremes to climate change is considered using results from theory, modeling, and observations, with a focus on the physical factors that control the response.
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Observed heavy precipitation increase confirms theory and early models

TL;DR: The authors used the intensification of heavy precipitation as a counterexample, where seemingly complex and potentially computationally intractable processes manifest themselves to first order in simple ways: heavy precipitation intensification is now emerging in the observed record across many regions of the world.
References
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Journal ArticleDOI

The Changing Character of Precipitation

TL;DR: In this article, precipitation intensity, duration, frequency, and phase are as much of concern as total amounts, as these factors determine the disposition of precipitation once it hits the ground and how much runs off.
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A European daily high-resolution gridded data set of surface temperature and precipitation for 1950-2006

TL;DR: In this paper, the authors presented a European land-only daily high-resolution gridded data set for precipitation and minimum, maximum, and mean surface temperature for the period 1950-2006.
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Constraints on future changes in climate and the hydrologic cycle

TL;DR: It will be substantially harder to quantify the range of possible changes in the hydrologic cycle than in global-mean temperature, both because the observations are less complete and because the physical constraints are weaker.
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A decade of weather extremes

TL;DR: In this paper, a review of the evidence so far, it is argued that certain events or an increase in their frequency can be linked with confidence to the human influence on climate.
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Atmospheric Warming and the Amplification of Precipitation Extremes

TL;DR: Observations reveal a distinct link between rainfall extremes and temperature, with heavy rain events increasing during warm periods and decreasing during cold periods, implying that projections of future changes in rainfall extremes in response to anthropogenic global warming may be underestimated.
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