-
Posts
44616 -
Joined
-
Last visited
-
Days Won
262
Everything posted by Phil
-
Good point. The flat ridge south of the Aleutians is actually a reflection of the descending (sinking) branch of the Pacific Hadley Cell. It's unusually broad/poleward right now, even by modern standards. Blah. Need to get that wave-1 tropical-convective signal back, which'll tilt the longitudinal IO/PAC Hadley Cell gradient, ousting the zonal Pacific Jet.
-
Mama Nature is trollolololing us.
-
In the raw, here's satellite-era weak/mod -ENSO Octobers that preceded blocky winters: http://i724.photobucket.com/albums/ww243/phillywillie/Mobile%20Uploads/60061ADF-85CA-4D47-AE78-29DA7CE30FC9_zpsffbktryz.png Versus those that preceded zonal winters. Not a huge difference, except over Eurasia/NE Siberia: http://i724.photobucket.com/albums/ww243/phillywillie/Mobile%20Uploads/DF431A14-5778-435A-B9FD-81E3A77A399D_zpsa8zesbc6.png Difference: Eurasian gradient and EPO still predictors: http://i724.photobucket.com/albums/ww243/phillywillie/Mobile%20Uploads/26DFFE6C-7AD9-4E97-A19A-9FF13BD062D3_zpsnrgrhgvt.png
-
Many of the -ENSO/+QBO analogs delivered in February, as well. I highly doubt this is a one-and-done winter, given what will probably be a highly variable/transient pattern progression. If there's one thing I'm confident of in regards to this winter, it's a highly variable, unstable pattern progression. This background state is just too weak to constrain things much, IMO.
-
I'm not even looking into it like that. I don't think it matters in relation to winter, given it's probably an emergent intraseasonal-scale excursion, similar to the one that occurred for a few weeks in August. It's just fascinating to me from a scientific standpoint, as these emergent behaviors are something I've been trying (and failing) to figure out for years.
-
This is funny, because current SSTAs are almost perfectly opposite. This is a good illustration of the distinction between the systematic background state, and intraseasonal forcing/feedback. The SSTAs don't constrain the atmosphere to a high frequency degree. They only constrain the lower frequency background tendencies. http://www.tropicaltidbits.com/analysis/ocean/cdas-sflux_ssta_global_1.png