We know this from the cross-ENSO interhemispheric signature in
annual earth rotation.
Not exact matches
It is found that the El Niño — Southern Oscillation (ENSO) is driven not only by the seasonal heating, but also by three more external periodicities (incommensurate to the
annual period) associated with the ~ 18.6 - year lunar - solar nutation of the
Earth rotation axis, ~ 11 - year sunspot activity cycle and the ~ 14 - month Chandler wobble in the
Earth's pole motion.
One finds on the secular time scale that both of the X - and Y - component temporal,
annual - means profiles of the Earth's Orientation mimic exactly the Global Temperature Anomaly (GTA) annual means profile On the decade time scale one finds that the GTA mimics the Geomagnetic Dipole variations and the variations in the Earths Anomalous Rotation Rate [i.e., Excess Length of Day (ELOD) Annual M
annual - means profiles of the
Earth's Orientation mimic exactly the Global Temperature Anomaly (GTA)
annual means profile On the decade time scale one finds that the GTA mimics the Geomagnetic Dipole variations and the variations in the Earths Anomalous Rotation Rate [i.e., Excess Length of Day (ELOD) Annual M
annual means profile On the decade time scale one finds that the GTA mimics the Geomagnetic Dipole variations and the variations in the
Earths Anomalous
Rotation Rate [i.e., Excess Length of Day (ELOD)
Annual M
Annual Means].
If you could position yourself to view the
earth's
rotation say 1M Km above the sub-solar point the weather (from east to west) would always look much the same, only varying (on any centennial timeframe) according to the sun's
annual declination and the consequent local geographical (land or ocean) effects.
The climatic seasons that we experience on
Earth are caused by a combination of
Earth's
annual orbit around the sun and its tilted axis of
rotation.
7 Movements of
Earth in Space (Page 270) The climatic seasons that we experience on
Earth are caused by a combination of
Earth's
annual orbit around the sun and its tilted axis of
rotation.