When they say dynamic they don't just
means changes in precipitation or temperature, but also changes in pressure and humidity.
Not exact matches
Widening of the tropics would also probably be associated with poleward movement of major extratropical climate zones due to
changes in the position of jet streams, storm tracks,
mean position of high and low pressure systems, and associated
precipitation regimes.
«Looking at
changes in the number of dry days per year is a new way of understanding how climate
change will affect us that goes beyond just annual or seasonal
mean precipitation changes, and allows us to better adapt to and mitigate the impacts of local hydrological
changes,» said Polade, a postdoctoral researcher who works with Scripps climate scientists Dan Cayan, David Pierce, Alexander Gershunov, and Michael Dettinger, who are co-authors of the study.
The lakes they examined are so - called closed - basin lakes, which have rivers feeding into them, but not draining them,
meaning that
changes in lake levels are governed solely by
precipitation and evaporation.
This does not necessarily
mean the mechanisms driving
precipitation changes in climate models are wrong.
has decreased
in winter, but no significant
change in annual
mean precipitation potentially because of very slight increases
in spring and fall
precipitation;
precipitation is projected to increase across Montana, primarily
in spring; slight decrease
in summer
precipitation; variability of
precipitation year - to - year projected to increase
Her work focuses on the causes of
change in mean and extreme temperature and
precipitation.
For birds and amphibians, we considered exposure to five components of climate
change, namely
changes in mean temperature, temperature variability,
mean precipitation,
precipitation variability and sea level rise.
Here's the problem forests and forest managers face under climate
change: Increasing global
mean temperatures,
changes in precipitation, and the hydrologic cycle are expected to lead to temperature and drought stress for many tree species.
Statewide
precipitation has decreased
in winter (0.14 inches / decade -LSB--0.36 cm / decade]-RRB- since 1950, but no significant
change has occurred
in annual
mean precipitation, probably because of very slight increases
in spring and fall
precipitation.
«Thus
changes in the pattern of R could directly influence that of
precipitation, regardless of any impact on the global
mean radiation budget.»
A reduction
in the
precipitation area implies higher
mean precipitation intensity, and may be linked to
changes in the atmospheric overturning presented above.
They discussed the effect of variables being non-iid on the extreme value analysis, and after taking that into account, propose that
changes in extreme
precipitation are likely to be larger than the corresponding
changes in annual
mean precipitation under a global warming.
Fractional
changes in local
precipitation are expected to be larger than those
in the global
mean.
What I
mean by climate
change One definition of a climate
change is a shift
in the pdf describing the temperature,
precipitation, or some other variable.
Further,
precipitation over land is a small fraction of the total, so there's a lot of room for
changes in precip there without altering the result on the global
mean.
Decreases
in precipitation over many subtropical areas are evident
in the multi-model ensemble
mean, and consistency
in the sign of
change among the models is often high (Wang, 2005), particularly
in some regions like the tropical Central American - Caribbean (Neelin et al., 2006).
The net
change over land accounts for 24 % of the global
mean increase
in precipitation, a little less than the areal proportion of land (29 %).
The global map of the A1B 2080 to 2099
change in annual
mean precipitation is shown
in Figure 10.12, along with other hydrological quantities from the multi-model ensemble.
In GCMs, the global mean evaporation changes closely balance the precipitation change, but not locally because of changes in the atmospheric transport of water vapou
In GCMs, the global
mean evaporation
changes closely balance the
precipitation change, but not locally because of
changes in the atmospheric transport of water vapou
in the atmospheric transport of water vapour.
As for how this could be — and
in light of the findings of the references listed above — Rankl et al. reasoned that «considering increasing
precipitation in winter and decreasing summer
mean and minimum temperatures across the upper Indus Basin since the 1960s,» plus the «short response times of small glaciers,» it is only logical to conclude that these facts «suggest a shift from negative to balanced or positive mass budgets
in the 1980s or 1990s or even earlier, induced by
changing climatic conditions since the 1960s.»
At the same time,
precipitation patterns are also
changing all over the planet;
in the Arctic, that
means more erratic snowfall.
Although there is as yet no convincing evidence
in the observed record of
changes in tropical cyclone behaviour, a synthesis of the recent model results indicates that, for the future warmer climate, tropical cyclones will show increased peak wind speed and increased
mean and peak
precipitation intensities.
Bonfils, C.J.W., B.D. Santer, T.J. Phillips, K. Marvel, L.R. Leung, C. Doutriaux, and A. Capotondi, 2015: Relative contributions of
mean - state shifts and ENSO - driven variability to
precipitation changes in a warming climate.
A comparison of the long term and short term
mean for monthly
precipitation and temperature from the eight NOAA State of Washington Division 5 Weather Stations (Cascade Mountains) illustrates three important climate
changes in the North Cascades for the 1984 - 1994 period.
Models disagree on annual
mean precipitation changes in the NA monsoon region.
Understanding how the global -
mean precipitation rate will
change in response to a climate forcing is a useful thing to know.
Overall, the scientists found that
precipitation extremes of different kinds will occur, with only small
changes in the
mean precipitation across the rainy season.
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).
«What that
means is that it's actually possible
in many cases for the response of
precipitation to climate
change to be quite different from place to place.»
The NAO's prominent upward trend from the 1950s to the 1990s caused large regional
changes in air temperature,
precipitation, wind and storminess, with accompanying impacts on marine and terrestrial ecosystems, and contributed to the accelerated rise
in global
mean surface temperature (e.g., Hurrell 1996; Ottersen et al. 2001; Thompson et al. 2000; Visbeck et al. 2003; Stenseth et al. 2003).
Increase
in heavy
precipitation events
in mid-latitudes, disproportionate with
changes in mean (1951 - 2003)[AR4 3.8.2.2]
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.»
Choi and Fisher (2003) estimated the expected
change in flood damages for selected USA regions under two climate -
change scenarios
in which
mean annual
precipitation increased by 13.5 % and 21.5 %, respectively, with the standard deviation of annual
precipitation either remaining unchanged or increasing proportionally.
In the coming century, increasing atmospheric GHG concentration and associated warming could have important hydrological and water resource consequences in the Southwest resulting from mean state changes due to higher evaporation and decreased precipitation [73 — 75
In the coming century, increasing atmospheric GHG concentration and associated warming could have important hydrological and water resource consequences
in the Southwest resulting from mean state changes due to higher evaporation and decreased precipitation [73 — 75
in the Southwest resulting from
mean state
changes due to higher evaporation and decreased
precipitation [73 — 75].
Global solar irradiance reconstruction [48 — 50] and ice - core based sulfate (SO4) influx
in the Northern Hemisphere [51] from volcanic activity (a);
mean annual temperature (MAT) reconstructions for the Northern Hemisphere [52], North America [29], and the American Southwest * expressed as anomalies based on 1961 — 1990 temperature averages (b);
changes in ENSO - related variability based on El Junco diatom record [41], oxygen isotopes records from Palmyra [42], and the unified ENSO proxy [UEP; 23](c);
changes in PDSI variability for the American Southwest (d), and
changes in winter
precipitation variability as simulated by CESM model ensembles 2 to 5 [43].
The figure below shows the
change in precipitation and evaporation (which have to balance globally) against the global
mean surface temperature
change.
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].
These figures illustrate the way the probability distribution of future global
mean temperature
change under a high - emissions scenario is linked to different potential
changes in temperature and
precipitation at a county - level.
Multi-model
mean changes in surface air temperature (°C, left),
precipitation (mm day — 1, middle) and sea level pressure (hPa, right) for boreal winter (DJF, top) and summer (JJA, bottom).
The authors tried to constrain the global -
mean future
precipitation change simulated by the set of climate models participating
in the CMIP2 model intercomparison project through observable temperature variability and a simple energetic framework.
This low
precipitation period, on top of the steady seasonal drought, permitted an extreme drought stress study that acknowledges the important role of climate extremes (rather than
changes in the
mean)
in tree function (Reyer et al. 2012).
However, considerable evidence (8 ⇓ ⇓ — 11, 31 ⇓ — 33) simultaneously suggests that the response of northeastern Pacific atmospheric circulation to anthropogenic warming is likely to be complex and spatiotemporally inhomogeneous, and that
changes in the atmospheric
mean state may not be reflective of
changes in the risk of extreme events (including atmospheric configurations conducive to
precipitation extremes).
Another aspect of these projected
changes is that wet extremes are projected to become more severe
in many areas where
mean precipitation is expected to increase, and dry extremes are projected to become more severe
in areas where
mean precipitation is projected to decrease.
This study seeks to explain the effects of cloud on
changes in atmospheric radiative absorption that largely balance
changes in global
mean precipitation under climate
change.
Over West Africa, AOGCM - simulated
changes in annual
mean precipitation are about 5 to 10 % larger than for atmosphere - only simulations, and
in better agreement with data reconstructions (Braconnot et al., 2004).
She continues by observing that «it is likely that both extreme weather events (storms, floods, heat waves) and
changes in mean temperatures,
precipitation and sea - levels will
in many cases contribute to increasing levels of mobility.»
If a shift
in the hydrological cycle were to lower the response
in the global
mean temperature, there may be a poisonous sting
in such a negative feedback:
changes in the
precipitation patterns.
The patterns and magnitude of the
precipitation changes (scaled to a global
mean warming of 4 °C) are similar
in the high - end and non-high-end models, although the reductions
in precipitation tend to be slightly greater
in the high - end models.
Precipitation changes (%)
in (a, b) DJF and (c, d) JJA from the median of the A2 ensemble, after scaling to 4 °C global
mean warming
in all cases.