The working hypothesis of this study is that periodic lunar nodal tides and almost periodic solar radiation variations influence sea level changes through their harmonic beating of nearby natural and/or forced broadband oscillations of the sea level at multi-decadal frequencies. The presence of the harmonics of the lunar nodal tides and the solar radiation variations, including the pole tides, is investigated by modeling and estimating the amplitudes of the corresponding periodicities in 27 globally distributed long tide gauge records. Statistically significant signatures of sub and superharmonics of lunar nodal tides and forced sea level variations due to solar radiation are detected in all station records.Meta-analysis of the harmonic amp...
The article describes lunar daily and lunar monthly oscillations in ƒ0F2 and H at Huancayo for ...
It has been known for many decades that the lunar tidal influence in the equatorial electrojet (EEJ...
A numerical model has been used to calculate the atmospheric response to forcing at periods in the r...
The residuals of 27 globally distributed long tide gauge recordswere scrutinized after removing the ...
The link between secular changes in the lunar semidiurnal ocean tide (M2) and relative sea level ris...
During the last century the response of the oceans to tidal forces has changed significantly. This ...
The periodic movement of the Earth, the Moon, and the Sun determines the variety and type of sea tid...
It seems that the wind shear theory is accepted for the explanation of sporadic E at mid and low la...
During the PSMOS Global-scale tidal variability experiment campaign of June 1-August 31, 1999, a net...
Tides are a consequence of the gravitational pull of the Moon and the Sun exerted on the waters of t...
15th MST Radar WorkshopSession M6: Middle atmosphere dynamics and structureMay 31 (Wed), NIPR Audito...
The lunar semidiurnal tide in winds measured at around 90 km altitude has been isolated with amplit...
During the PSMOS Global-scale tidal variability experiment campaign of June 1–August 31, 1999, a net...
Previous studies have demonstrated that tides are subject to considerable changes on secular time sc...
In this paper we investigate the correlation between the atmospheric perturbations at Paranal Obser...
The article describes lunar daily and lunar monthly oscillations in ƒ0F2 and H at Huancayo for ...
It has been known for many decades that the lunar tidal influence in the equatorial electrojet (EEJ...
A numerical model has been used to calculate the atmospheric response to forcing at periods in the r...
The residuals of 27 globally distributed long tide gauge recordswere scrutinized after removing the ...
The link between secular changes in the lunar semidiurnal ocean tide (M2) and relative sea level ris...
During the last century the response of the oceans to tidal forces has changed significantly. This ...
The periodic movement of the Earth, the Moon, and the Sun determines the variety and type of sea tid...
It seems that the wind shear theory is accepted for the explanation of sporadic E at mid and low la...
During the PSMOS Global-scale tidal variability experiment campaign of June 1-August 31, 1999, a net...
Tides are a consequence of the gravitational pull of the Moon and the Sun exerted on the waters of t...
15th MST Radar WorkshopSession M6: Middle atmosphere dynamics and structureMay 31 (Wed), NIPR Audito...
The lunar semidiurnal tide in winds measured at around 90 km altitude has been isolated with amplit...
During the PSMOS Global-scale tidal variability experiment campaign of June 1–August 31, 1999, a net...
Previous studies have demonstrated that tides are subject to considerable changes on secular time sc...
In this paper we investigate the correlation between the atmospheric perturbations at Paranal Obser...
The article describes lunar daily and lunar monthly oscillations in ƒ0F2 and H at Huancayo for ...
It has been known for many decades that the lunar tidal influence in the equatorial electrojet (EEJ...
A numerical model has been used to calculate the atmospheric response to forcing at periods in the r...