The surface climate response to 11-yr solar forcing during northern winter is first reestimated by applying a multiple linear regression (MLR) statistical model to Hadley Centre sea level pressure (SLP) and sea surface temperature (SST) data over the 1880–2009 period. In addition to a significant positive SLP response in the North Pacific found in previous studies, a positive SST response is obtained across the midlatitude North Pacific. Negative but insignificant SLP responses are obtained in the Arctic. The derived SLP response at zero lag therefore resembles a positive phase of the Arctic Oscillation (AO). Evaluation of the SLP and SST responses as a function of phase lag indicates that the response evolves from a negative AO-like mode a...
The Arctic Oscillation (AO) is the leading climate mode of sea level pressure (SLP) anomalies during...
The surface response to 11 year solar cycle variations is investigated by analyzing the long-term me...
Differences between two ensembles of Goddard Earth Observing System Chemistry-Climate Model simulati...
The origin of the tropical lower-stratospheric response to 11-yr solar forcing and its possible coup...
International audienceThe impact of the 11-year solar cycle on the stratosphere and, in particular, ...
International audienceTwo temperature datasets are analyzed for quantifying the 11-year solar cycle ...
The surface response to the 11 year solar cycle is assessed in ensemble simulations of the twentieth...
The role of stratospheric ozone changes in determining the climate response to solar forcing is inve...
The surface response to the 11-yr solar cycle is assessed in ensemble simulations of the 20th centur...
The ECHAM 3.2 (T21), ECHAM 4 (T30) and LMD (version 6, grid-point resolution with 96 longitudes × 72...
The 11 year solar‐cycle component of climate variability is assessed in historical simulations of mo...
We report a series of experiments to explore clima~ responses to two types of solar spectral forcing...
[1] Links between autumn-winter snow anomalies over North America and winter climate parameters thro...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
An influence of solar irradiance variations on Earth's surface climate has been repeatedly suggested...
The Arctic Oscillation (AO) is the leading climate mode of sea level pressure (SLP) anomalies during...
The surface response to 11 year solar cycle variations is investigated by analyzing the long-term me...
Differences between two ensembles of Goddard Earth Observing System Chemistry-Climate Model simulati...
The origin of the tropical lower-stratospheric response to 11-yr solar forcing and its possible coup...
International audienceThe impact of the 11-year solar cycle on the stratosphere and, in particular, ...
International audienceTwo temperature datasets are analyzed for quantifying the 11-year solar cycle ...
The surface response to the 11 year solar cycle is assessed in ensemble simulations of the twentieth...
The role of stratospheric ozone changes in determining the climate response to solar forcing is inve...
The surface response to the 11-yr solar cycle is assessed in ensemble simulations of the 20th centur...
The ECHAM 3.2 (T21), ECHAM 4 (T30) and LMD (version 6, grid-point resolution with 96 longitudes × 72...
The 11 year solar‐cycle component of climate variability is assessed in historical simulations of mo...
We report a series of experiments to explore clima~ responses to two types of solar spectral forcing...
[1] Links between autumn-winter snow anomalies over North America and winter climate parameters thro...
The 11 year solar-cycle component of climate variability is assessed in historical simulations of mo...
An influence of solar irradiance variations on Earth's surface climate has been repeatedly suggested...
The Arctic Oscillation (AO) is the leading climate mode of sea level pressure (SLP) anomalies during...
The surface response to 11 year solar cycle variations is investigated by analyzing the long-term me...
Differences between two ensembles of Goddard Earth Observing System Chemistry-Climate Model simulati...