«Warming in California has made it more probable that when a low precipitation year occurs,
it occurs in warm conditions and is more likely to produce severe drought,» said lead study author Noah Diffenbaugh, an associate professor in the School of Earth Sciences at Stanford.
Not exact matches
In the southern California avocado growing areas, from San Luis Obispo County to San Diego County, drier than normal
conditions and
warmer days
occur through March 30th.
In the Near Term — March 29 - April 12...
In the southern California avocado growing areas, from San Luis Obispo County to San Diego County, drier than normal
conditions and
warmer days
occur through March 30th.
The strength and path of the North Atlantic jet stream and the Greenland blocking phenomena appear to be influenced by increasing temperatures
in the Arctic which have averaged at least twice the global
warming rate over the past two decades, suggesting that those marked changes may be a key factor affecting extreme weather
conditions over the UK, although an Arctic connection may not
occur each year.
Crocodiles
occur in tropical climates, and they are frequently used as markers of
warm conditions when they are found as fossils.
If the same
conditions that caused the storm had
occurred in a world without the
warming observed over the last century, it would not have been as severe.
This chemical weathering process is too slow to damp out shorter - term fluctuations, and there are some complexities — glaciation can enhance the mechanical erosion that provides surface area for chemical weathering (some of which may be realized after a time delay — ie when the subsequent
warming occurs — dramatically snow
in a Snowball Earth scenario, where the frigid
conditions essentially shut down all chemical weathering, allowing CO2 to build up to the point where it thaws the equatorial region, at which point runaway albedo feedback drives the Earth into a carbonic acid sauna, which ends via rapid carbonate rock formation), while lower sea level may increase the oxidation of organic C
in sediments but also provide more land surface for erosion... etc..
It is especially common
in warmer climates, though can still
occur in cooler rainy
conditions.
Accessibility to the dive sites, such as Lighthouse Reef, Turneffe Islands, as well as many excellent sites right off Ambergris Caye, combined with excellent weather
conditions, clear
warm water, the variety of dive sites and
in the unlikely chance that a diving accident should
occur, the hyperbaric chamber is minutes away from any of the dive sites.
Runaway greenhouse
warming can
occur for really extreme
conditions (Venus at present, Earth
in maybe 5 billion years time when the sun becomes a red giant), but is not a possibility for the next hundred years.
Due to favorable
warm and wet weather
conditions in spring 2010 the mass growth of these annual Brassicacea species
occurred on a big scale.
Bleaching
occurs when these colorful algae die out or leave the polyps, often
in response to overly
warm conditions.
Rising temperatures lead to an increase
in vector - borne and water - borne diseases (due to more transmission
occurring in higher rainfall and increased reproduction of vectors
in warmer conditions).
Conditions like this
occurred at the peaks of every
warm period
in the past ten thousand years.
@ - Herman Alexander Pope»
Conditions like this
occurred at the peaks of every
warm period
in the past ten thousand years.
If these
warm ocean temperatures
occur in combination with abnormally
warm conditions near Alaska, the extra heat from the Arctic can intensify the ridge, causing it to reach farther northward, become more persistent, and pump even more heat into the region near Alaska.
«The authors write that «the El Niño - Southern Oscillation (ENSO) is a naturally
occurring fluctuation,» whereby «on a timescale of two to seven years, the eastern equatorial Pacific climate varies between anomalously cold (La Niña) and
warm (El Niño)
conditions,» and that «these swings
in temperature are accompanied by changes
in the structure of the subsurface ocean, variability
in the strength of the equatorial easterly trade winds, shifts
in the position of atmospheric convection, and global teleconnection patterns associated with these changes that lead to variations
in rainfall and weather patterns
in many parts of the world,» which end up affecting «ecosystems, agriculture, freshwater supplies, hurricanes and other severe weather events worldwide.»»
The causal case is a cumulative case of: 1) correlation + 2) well - evidenced mechanism (i.e. plausibility) + 3) primacy, where the proposed cause
occurs before the effect + 4) robustness of the correlation under multiple tests /
conditions + 5) experimental evidence that adding the cause subsequently results
in the effect + 6) exclusion of other likely causes (see point 7 as well) + 7) specificity, where the effect having hallmarks of the cause (ex: the observed tropospheric
warming and stratopsheric cooling, is a hallmark of greenhouse - gas - induced
warming, not
warming from solar forcing) 8) a physical gradient (or a dose - response), where more of the cause produces a larger effect, or more of the cause is more likely to produce the effect +....
In this case, we can infer that not only one species but a community of plants
occurred at a high - elevation location ∼ 5000 yr ago under likely
warmer conditions.
An abrupt increase
in soot MARs
occurred in the early Holocene when an increase
in P. strobus indicated a
warmer, drier climate, and a decrease
in soot MARs subsequently
occurred when P. strobus declined and
warmer, more mesic
conditions prevailed.
Medieval
warm period (MWP), also called medieval
warm epoch or little climatic optimum, brief climatic interval that is hypothesized to have
occurred from approximately 900 ce to 1300 (roughly coinciding with the Middle Ages
in Europe),
in which relatively
warm conditions are said to have prevailed
in various parts of the world, though predominantly
in the Northern Hemisphere from Greenland eastward through Europe and parts of Asia.
«The
warming leads to a simulated long - term reduction
in soil moisture which, although of weak magnitude compared to soil moisture deficits induced by naturally
occurring droughts
in the southwest United States, would imply that drought
conditions may be entered more quickly and alleviated more slowly owing to long - term
warming... Radiative forcing of the climate system is another source of predictability, although not really a welcome one, and rising greenhouse gases will lead to a steady drying of southwest North America.
The convergence of prolonged
warming and arid
conditions suggests the mid-12th century may serve as a conservative analogue for severe droughts that might
occur in the future.
Taken together, the observed record from California suggests that (i) precipitation deficits are more likely to yield 1 - SD PMDI droughts if they
occur when
conditions are
warm and (ii) the occurrence of 1 - SD PMDI droughts, the probability of precipitation deficits producing 1 - SD PMDI droughts, and the probability of precipitation deficits co-occurring with
warm conditions have all been greater
in the past two decades than
in the preceding century.
«We've seen the effects of record heat on snow and soil moisture this year
in California, and we know from this new research that climate change is increasing the probability of those
warm and dry
conditions occurring together.»
Weather
conditions similar to 2012
occurred in the winter of 1942, when the U.S. Midwest was unusually
warm, and when the Wehrmacht encountered the formidable forces of «General Frost»
in a Russian winter not unlike the one Russians just had.
These ocean upwelling
conditions occur beneath a complementary downwelling branch of the atmosphere's Hadley circulation — a planetary - scale flow pattern
in both hemispheres that takes humid air ascending at low latitudes, heats and desiccates it
in deep precipitating tropical clouds, and then sinks it at midlatitudes, where it is considerably
warmer and drier than it was.
There are a variety of factors that are known to make for quiet Atlantic hurricane seasons — particularly the occurrence of El Nino
conditions (as
occurred in 2002)
in the Pacific Ocean, characterized by very
warm tropical ocean waters.
Although we can not say at present whether more or fewer hurricanes will
occur in the future with global
warming, the hurricanes that do
occur near the end of the 21st century are expected to be stronger and have significantly more intense rainfall than under present day climate
conditions.
It is important to note that Lamb also considered the
warmest conditions to have
occurred at different times
in different areas: between 950 and 1200
in European Russia and Greenland, but somewhat later, between 1150 and 1300 (though with notable warmth also
in the later 900s)
in most of Europe (Lamb, 1977).