La Niña favors
a jet stream pattern which more consistently sends storms into the Pacific Northwest, leaving the Southwest drier than normal.
Not exact matches
«The
jet stream changes character every 10 to 12 days, and we use this
pattern to predict the weather,» said Anthony Lupo, professor of atmospheric science in MU's School of Natural Resources,
which is located in the College of Agriculture, Food and Natural Resources.
The disruption to that wind
pattern can reverberate through the atmosphere, impacting the flow of air from the equator to the poles,
which in turn can affect the
jet stream and weather around the globe.
Large belts and zones form a consistent
pattern of
jet streams which give the planet its familiar striped appearance.
There is some evidence that a warming world will affect
jet stream patterns,
which control the speed and direction of weather systems.
The temperature differential between the cold of the far North and the warmer air of the temperate zones to the south fuel the
jet stream,
which steers weather
patterns in the Northern Hemisphere.
This shifts around wind
patterns there and has a domino effect through the atmosphere; over the U.S., it causes a shift in the position of the wintertime
jet stream,
which controls how storms move across the country.
«The idea is that ice loss in this area tends to create a wavier
jet stream pattern,
which causes colder winters in central Asia and blocking
patterns that make this weather regime very persistent.»
The current La Nina event and natural variability are also involved, and it is difficult to say
which effect is mostly responsible for the current
jet stream pattern.
Reading the numerous references there is clear evidence of «blocking
patterns,» perhaps as the
jet stream shifts, or a high pressure takes up residence, feeding in winds from a certain direction
which generally shape British weather.»
First, the west - to - east
jet stream appears to be slowing down,
which allows weather
patterns to persist in certain areas for longer.
4) A change in global weather
patterns which I noticed as long ago as 2000 whereby the
jet streams moved back towards the equator from the positions they adopted during the warming spell.
A strong El Niño heats up the atmosphere and changes circulation
patterns around the globe, especially the
jet stream over the Pacific,
which becomes stronger and dumps more frequent and intense storms over the western U.S., especially California.
Because these waves in the
jet stream were so big, Francis says, that
pattern became very powerful,
which is why it persisted for so long.
As the air gets hotter, thunderstorms are more likely to develop in the area, the energy of
which fluctuates the
jet stream and creates a high - low or «dipole,» pressure
pattern.
This, in turn, causes disruptions in the
jet stream which brings huge fluctuations in local weather
patterns — of highs AND lows, precipitation AND drought.
Examination of daily ozone and
jet stream satellite data reveals a process
which responds to wandering magnetic poles
which affect
jet streams and Rossby wave loops to exacerbate extreme weather
patterns and cause global climate change.
The
pattern is also associated with the negative phase of the Arctic Oscillation,
which is the dominant atmospheric
pattern observed during severe winters and comprises a weakened
jet stream and more cold air intrusions southward from the Arctic into North America and Eurasia.
The new study, along with other previously published research, showed that the decline in sea ice and snow cover has slowed the west - to - easterly component of the
jet stream, thereby enhancing the north - to - south waviness of the
jet,
which leads to the creation of more stagnant or «blocked» weather
patterns.
A negative AO changes pressure
patterns at higher latitudes
which influence the shape of the
jet stream.
We found that relative to the global - mean trends of the respective layers, both hemispheres have experienced enhanced tropospheric warming and stratospheric cooling in the 15 to 45 ° latitude belt,
which is a
pattern indicative of a widening of the tropical circulation and a poleward shift of the tropospheric
jet streams and their associated subtropical dry zones.