Scaling regimes and linear/nonlinear responses of last millennium climate to volcanic and solar forcings
At scales much longer than the deterministic predictability limits (about 10 days), the statistics of the atmosphere undergoes a drastic transition, the high-frequency weather acts as a random forcing on the lower-frequency macroweather. In addition, up to decadal and centennial scales the equivalen...
Main Authors: | S. Lovejoy, C. Varotsos |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-02-01
|
Series: | Earth System Dynamics |
Online Access: | http://www.earth-syst-dynam.net/7/133/2016/esd-7-133-2016.pdf |
Similar Items
-
Comment on "Scaling regimes and linear/nonlinear responses of last millennium
climate to volcanic and solar forcing" by S. Lovejoy and C. Varotsos (2016)
by: K. Rypdal, et al.
Published: (2016-07-01) -
Hemispherically asymmetric volcanic forcing of tropical hydroclimate during
the last millennium
by: C. M. Colose, et al.
Published: (2016-08-01) -
Mechanisms for European summer temperature response to solar forcing over the last millennium
by: D. Swingedouw, et al.
Published: (2012-10-01) -
Volcanic impact on the Atlantic Ocean over the last millennium
by: J. Mignot, et al.
Published: (2011-12-01) -
Assessing the impact of large volcanic eruptions of the last millennium (850–1850 CE) on Australian rainfall regimes
by: S. A. P. Blake, et al.
Published: (2018-06-01)