By one measure (the EQSOI), the El Niño -
related changes in the atmospheric circulation in 1997/98 and 2015/16 are tied; by another (the SOI), 1997/98 was stronger.
Not exact matches
In a series of papers, we've shown that the warmer temperatures observed over the WAIS are the result of those same atmospheric circulation changes, which are not related to the SAM, but rather to the remote forcing from changes in the tropical Pacific: changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
In a series of papers, we've shown that the warmer temperatures observed over the WAIS are the result of those same
atmospheric circulation changes, which are not
related to the SAM, but rather to the remote forcing from
changes in the tropical Pacific: changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
in the tropical Pacific:
changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012).
The
changes include
changes in the TOA energy dynamic
related to
changes in ocean and
atmospheric circulation —
changes in cloud.
In models at least, this kind of response would be most directly related to increases in stratification due to surface warming, as I understand it, and not directly to the kind of change in atmospheric circulation discussed in Dian's pape
In models at least, this kind of response would be most directly
related to increases
in stratification due to surface warming, as I understand it, and not directly to the kind of change in atmospheric circulation discussed in Dian's pape
in stratification due to surface warming, as I understand it, and not directly to the kind of
change in atmospheric circulation discussed in Dian's pape
in atmospheric circulation discussed
in Dian's pape
in Dian's paper.
What science is suggesting is that there are multi-decadal regimes that are
related to
changes in ocean and
atmospheric circulation in the broader Earth system.
One last point
related to my last post, is the extent / degree of magnitude of a more meridional
atmospheric circulation pattern (N.H. especially) could influence snow cover, cloud cover, and precipitation amounts which could set up stronger positive climatic feedbacks, which could then result
in an even more significant climatic
change going forward.
Shows that the
changes in discharge extremes are
related to the regional pluriannual rainfall variability and the associated
atmospheric circulation as well as to tropical large - scale climatic indicators
The seasonal climate may
relate to
changes in the ocean
circulation pattern prior to 4.6 Ma that resulted
in an increased temperature and
atmospheric pressure gradient between the east coast of North America and the Atlantic Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier conditions.