Citation: Soon, W.H., E.S. Posmentier, and S.L. Baliunas, 1996: Inference of solar
irradiance variability from terrestrial temperature changes, 1880 - 1993: An astrophysical application of the Sun - climate connection.
Not exact matches
The solar UV
irradiance from the thermosphere of Saturn and the solar wind are the most probable sources to account for the long - term
variability of the electron radiation belts (Roussos et al. 2014), suggesting that external drivers play indeed an important role in Saturn's magnetospheric dynamics.
Contributions
from the following topics (but not exclusively) are invited: • Solar
irradiance and energetic particle impacts on the atmosphere • Upper atmospheric dynamical
variability and coupling between atmospheric layers • Solar variations and stratosphere - troposphere coupling • Solar influence on climate
variability • Solar
irradiance (spectral and total
irradiance) variations
from «Magnitudes and Timescales of Total Solar
Irradiance Variability,» by Greg Kopp.
Since the solar UV
irradiance has no long - term trend, the mechanism for the secular change of TSI must differ
from the effect of surface magnetism, as manifested by sunspots, faculae, and network which indeed explain well the intra-cycle
variability of both total and spectral
irradiance.
The temperature trend since 1998 is understood to result
from natural climate
variability, combined with reduced solar
irradiance during the downward part of the solar cycle after its 2001 maximum.
«
From what I can tell, the list was compiled mostly from reviewed scientific articles in which authors proposed or identified various sources of natural variability in climate; in my case solar irradiance and cosmic ray f
From what I can tell, the list was compiled mostly
from reviewed scientific articles in which authors proposed or identified various sources of natural variability in climate; in my case solar irradiance and cosmic ray f
from reviewed scientific articles in which authors proposed or identified various sources of natural
variability in climate; in my case solar
irradiance and cosmic ray flux.
Global solar
irradiance reconstruction [48 — 50] and ice - core based sulfate (SO4) influx in the Northern Hemisphere [51]
from volcanic activity (a); mean annual temperature (MAT) reconstructions for the Northern Hemisphere [52], North America [29], and the American Southwest * expressed as anomalies based on 1961 — 1990 temperature averages (b); changes in ENSO - related
variability based on El Junco diatom record [41], oxygen isotopes records
from Palmyra [42], and the unified ENSO proxy [UEP; 23](c); changes in PDSI
variability for the American Southwest (d), and changes in winter precipitation
variability as simulated by CESM model ensembles 2 to 5 [43].
Phase relationships between hemispheric and global climate reconstructions
from tree - rings and the solar
irradiance time series indicate a lag of ~ 10 years (range, 5 - 20 years), with solar changes leading temperature anomalies, consistent with both climate modeling and other climate and solar
variability studies (Eichler et al., 2009; Breitenmoser et al., 2012; Anchukaitis et al., 2017).
Magnetic field indices derived
from synoptic magnetograms of the Mt. Wilson Observatory, i.e. Magnetic Plage Strength Index (MPSI) and Mt. Wilson Sunspot Index (MWSI), are used to study the effects of surface magnetism on total solar
irradiance variability during solar cycles 21, 22 and 23.