Sentences with phrase «precipitation change between»

Large differences in regional precipitation change between a first and second 2K of global warming.
The differences in precipitation changes between the high - end and non-high-end models in DJF and JJA were also investigated (data not shown).

Not exact matches

Although the study does not directly identify a link between this type of variation and current climate change vulnerability, these precipitation - linked variables could be a source of vulnerability in the future, Bay and her colleagues noted.
The results show that the correlation between climate change — i.e. the variation in temperature and precipitation between glacials and interglacials — and the loss of megafauna is weak, and can only be seen in one sub-region, namely Eurasia (Europe and Asia).
At the top the trend in annual measured precipitation between 1951 and 2010 is shown from the last scientific report of the Intergovernmental Panel on Climate Change (IPCC).
The team of researchers analyzed deposits of wind - blown dust called red clay that accumulated between six million and two and a half million years ago in north central China, adjacent to the Tibetan plateau, and used them to reconstruct changing monsoon precipitation and temperature.
Evidence from glacial advance / retreat (e.g. the evidence from tropical Andean glaciers you cite above) is often difficult to interpret, because glacial mass balance represents in general a subtle competition between the influences of ablation (determined by changes in temperature thresholds reached) and accumulation (determined by changes in humidity and precipitation).
Discussion of the Results: The results show that there is good connection between ENSO events and the changes in the background temperature and the precipitation in Nigeria.
Despite no historical changes in average annual precipitation between 1950 and 2015, there have been changes in average seasonal precipitation over the same period.
A model by the Purdue Climate Change Research Center in West Lafayette forecasts, by 2050, the full growing seasons will expand by one month; there will be 33 to 45 more days with temperatures above 90 degrees; an increase in precipitation between 14 percent and 22 percent; and 24 days to 36 days less snow cover.
Changes in aridity — the ratio between evaporation and precipitation — are expected in many regions as a result of climate change.
Recognizing that the impacts of changes in the frequency and intensity of these storms can easily exceed the impacts of changes in average temperature or precipitation, climate scientists are actively researching the connections between climate change and severe storms.
This can be affected by warming temperatures, but also by changes in snowfall, increases in solar radiation absorption due to a decrease in cloud cover, and increases in the water vapor content of air near the earth's surface.2, 14,15,16,17 In Cordillera Blanca, Peru, for example, one study of glacier retreat between 1930 and 1950 linked the retreat to a decline in cloud cover and precipitation.18
c, Measurements of July to September air temperature and annual precipitation changes at each site between 2003 and 2002.
Rather, winter precipitation has fluctuated between droughts and pluvials in these watersheds in the last century with no evidence of directional change, a pattern that has reoccurred in the southwestern United States for the last 1000 years [50].
The relationship between SSTs and spatial gradients in changes in (extreme) precipitation is an important finding for analysing necessary measures to anticipate future changes in the spatial and temporal distribution of rainfall in the country.
Oerlemans and Fortuin (1992) derived an empirical relationship between the mass balance sensitivity of a glacier to temperature change and the local average precipitation, which is the principal factor determining its mass turnover rate.
Given the conservative nature of the shape parameter, it is possible to illustrate the relationships between changes in the mean total precipitation, the probability of precipitation (which is proportional to the number of days with precipitation), and changes in heavy precipitation (Figure 2.34).
For a example, phase change which in the atmosphere mainly concerns evaporation of water at the surface (or boundary between surface and the fluid atmosphere) and condensation in the various layers of the atmosphere leading to cloud formation and precipitation.
Levels in some lakes represent a changing balance between inputs and outputs and, under one transient scenario, levels in Lake Victoria would initially fall as increases in evaporation offset changes in precipitation, but subsequently rise as the effects of increased precipitation overtake the effects of higher evaporation (Tate et al., 2004).
Between 1958 and 2007, New England saw a 67 percent increase in heavy precipitation events and the Midwest experienced a 31 percent increase, according to the 2009 federal report «Global Climate Change Impacts in the United States.»
A sentence in Chapter 13 of the 2007 IPCC Fourth Assessment Report on Impacts, Adaptation and Vulnerability states: «Up to 40 percent of the Amazonian forests could react drastically to even a slight reduction in precipitation; this means that the tropical vegetation, hydrology and climate system in South America could change very rapidly to another steady state, not necessarily producing gradual changes between the current and the future situation.»
The multiple physical connections between lightning, convection, precipitation, and rapid storm intensity changes make lightning a rich source of information on how these storms evolve.
It is important to recognize that ΔMLT is a proxy for changing magnitudes of temperature, precipitation, humidity, and CO2, and that both climate and ecosystem inertia also play roles in the relationships between climate forcing and vegetation responses.
The team used changes in dust levels and stable water isotopes in the annual ice layers of the two - mile - long Greenland ice core, which was hauled from the massive ice sheet between 1998 to 2004, to chart past temperature and precipitation swings.
That is particularly the case in California, where decadal precipitation variance is typically equivalent to 20 — 50 % of mean annual averages, mostly because of changes in precipitation received between November and March [16 — 17].
Climate change by 2060 was computed as the difference (air temperature) or ratio (precipitation and solar radiation) of monthly mean climate between the GCM (unforced) control and 2xCO2 simulations at GCM grid boxes coinciding with the crop modelling sites (Figure 13.1 b).
The basin could experience more precipitation with climate change, or bigger swings between wet and dry years or possibly even longer, more severe «megadroughts.»
«Climate change could influence monsoon dynamics and cause lower summer precipitation, a delay to the start of the monsoon season and longer breaks between the rainy periods.»
But the point is that, such a cascade doesn't want us to understand simply the relationship between increased precipitation and mosquitoes, but between climate change and death.
Modest and slowly evolving changes in the width of the Hadley Cell could force rapid changes in precipitation in transition regions that lie between the subtropical deserts and tropical rainforests (e.g., the Sahel).
Process - based studies have focused on understanding the role of the land surface on climate, with research looking into the regional impact of historical or hypothetical (future scenario) land - use change on climate, as well as understanding diurnal - scale relationships between surface fluxes of heat and moisture and subsequent atmospheric processes such as convection and the generation of precipitation.
This will provide an additional boost to temperature rises (and SLR and changes in precipitation patters) the next time the stars are lined up as they were in the period between 1976 and 1998.
Perry, C.A., 1992, A Correlation between precipitation in the Western United States and solar - irradiance variations, in Proceedings of the American Water Resources Association Conference Managing Water Resources During Climate Change, Reno, Nevada, November 1 - 6, p. 721 - 729.
They confirm that the incidence of illnesses is strongly associated with sharp changes in temperature and precipitation between seasons.
Spaceindustrynews: Mid-elevation forests — those between approximately 6,500 to 8,000 feet (1,981 to 2,438 meters) in elevation — are the most sensitive to rising temperatures and changes in precipitation and snowmelt associated with climate change, finds a new University of Colorado Boulder - led study co-funded by NASA.
This isn't just an educated guess — past societies have collapsed because of changes in temperature and precipitation... Brian Fagan documents the demise of the Pueblo Indian civilization at Chaco Canyon (in what's now New Mexico) during the Medieval Warm Period (roughly between 800 and 1300 A.D.).
By scaling the precipitation changes, the maps shown in figure 3 will illustrate any differences between the precipitation responses of the high - end and non-high-end models.
For example, analyses of glacier mass balances, volume changes and length variations along with temperature records in the western European Alps (Vincent et al., 2005) indicate that between 1760 and 1830, glacier advance was driven by precipitation that was 25 % above the 20th century average, while there was little difference in average temperatures.
Outside these areas, the sign and magnitude of projected changes varies between models, leading to substantial uncertainty in precipitation projections.
It seems clear to me that the sentence is about responses to a shift from one climate regime, the recent past and present day, to another, with less precipitation, in the future (it is the IPCC climate change impacts report after all, and they do say `... not necessarily producing gradual changes between the current and the future situation»).
«Up to 40 % of the Amazonian forests could react drastically to even a slight reduction in precipitation; this means that the tropical vegetation, hydrology and climate system in South America could change very rapidly to another steady state, not necessarily producing gradual changes between the current and the future situation (Rowell and Moore, 2000).»
The contested IPCC statement reads: «Up to 40 % of the Amazonian forests could react drastically to even a slight reduction in precipitation; this means that the tropical vegetation, hydrology and climate system in South America could change very rapidly to another steady state, not necessarily producing gradual changes between the current and the future situation (Rowell and Moore, 2000).»
There are a couple of lines in IPCC Working Group I («New coupled climate - carbon models (Betts et al., 2004; Huntingford et al., 2004) demonstrate the possibility of large feedbacks between future climate change and vegetation change, discussed further in Section 7.3.5 (i.e., a die back of Amazon vegetation and reductions in Amazon precipitation).»).
PRUDENCE RCM outputs showed non-linear relationships between mean maximum temperature and indices of drought and heatwave (Good et al., 2006), while changes in maximum 1 - day and 5 - day precipitation amounts were systematically enhanced relative to changes in seasonal mean precipitation across many regions of Europe (Beniston et al., 2007).
10 - 14 June 2013: CFMIP / EUCLIPSE Meeting on Cloud Processes and Climate Feedback, Hamburg, GERMANY Focus: Clouds and precipitation in a changing climate; Coupling between cloud processes and the atmospheric circulation; Ability of models to simulate cloud processes, and the impact of errors on model predictive capabilities
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