Results 151 to 160 of about 1,187,144 (257)
Modulation of the Mid‐Latitude Ionospheric Sporadic E Layer by the Northern Polar Vortex
Abstract The sporadic E (Es) layer is a prominent ionospheric irregularity mainly driven by vertical wind shear at mid‐latitudes. Hereby we statistically investigate for the first time Es responses to variations of the northern polar vortex (represented by NAM index) using long‐term ionosonde observations over Japan (44 years) and Australia (34 years).
Tomoki Maeda +3 more
wiley +1 more source
Post-2000 faster ENSO phase transitions amplify autumn sea ice loss in the Laptev-East Siberian Sea. [PDF]
Wang C +6 more
europepmc +1 more source
Abstract We examined projected changes in Madden–Julian Oscillation (MJO) teleconnections over North America using 90 ensemble members from the Community Earth System Model Version 2 Large Ensemble (CESM‐LENS2) under the SSP370 scenario. In the warmer climate, the classic PNA‐like teleconnection strengthens and shifts eastward, with large ensemble ...
Jingxuan Cui, Eric D. Maloney
wiley +1 more source
Present-day tropical precipitation and cloud feedbacks determine future equatorial Pacific trends. [PDF]
Stevenson S +6 more
europepmc +1 more source
Space–Time Spectral Analysis of the Southern Hemisphere Daily 500-hPa Geopotential Height
Cheng Sun, Jianping Li
semanticscholar +1 more source
Linking Hadley Cell Instability to Slow Equatorial Motions in Reanalysis and CMIP6 Models
Abstract A recent theory–originally proposed for tropical depression (TD)‐type waves–is extended to the Madden‐Julian Oscillation (MJO) and convectively‐coupled equatorial Rossby (ER) waves across the Indo‐Western Pacific region using reanalysis and Coupled Model Intercomparison Project Phase 6 (CMIP6) data. This framework posits that waves grow from a
Qiao‐Jun Lin +2 more
wiley +1 more source
Unfolding North American spring weather extremes along a scale ladder. [PDF]
Hwang J, You Z, Deng Y, Kim H.
europepmc +1 more source
A Climatological Spectral Study of the 500 mb Geopotential Height of the Northern Hemisphere.
M. Blackmon
semanticscholar +1 more source

