The solar proxy Be-10, measured in natural archives, has previously been assumed to lag solar activity by 1-2 yr. This reflects its residence time in the stratosphere where its main source lies. This study, based on a 30-yr global model simulation of the atmospheric transport of Be-10, shows that the stratospheric fraction of production varies significantly with the phase of solar activity. This leads to a lag between production change and deposition response of ca. 1 yr during the decreasing phase of solar activity but nearly no lag when solar activity increases. No lag is found for Be-7. The fraction of 10Be production in the stratosphere varies from ca. 65% to 69% between solar minimum (phi = 400 MV) and maximum (phi = 1200 MV), being hi...
Solar cycle activity effects (SCAE) in the lower and middle atmosphere, reported in several studies,...
Identification of the causes of past climate change requires detailed knowledge of one of the most i...
International audienceAims. The solar activity in the past millennia can only be reconstructed from ...
The solar proxy 10Be, measured in natural archives, has previously been assumed to lag solar activit...
Understanding the transport path of the solar activity proxy Be-10 from source to archive is crucial...
International audienceBeryllium-10 in ice provides a valuable proxy of solar activity. However, comp...
Ice core concentrations of Be-10 are used as a proxy for solar activity, but they might be affected ...
Reconstruction of solar irradiance has only been possible for the Holocene so far. During the last d...
The atmospheric production rate of the cosmogenic isotope 10Be is modulated by the solar wind. Spect...
Beryllium 10 concentrations (Be-10(con)) were measured at annual resolution from varved sediment cor...
10Be concentrations measured in ice cores exhibit larger temporal variability than expected based on...
International audienceMore than 2,000 analyses of beryllium-10 (Be-10) and sulfate concentrations we...
In a recent paper (Usoskin et al., 2002a), we have reconstructed the concentration of the cosmogenic...
International audienceAll existing 10Be records from Greenland and Antarctica show increasing concen...
Solar cycle activity effects (SCAE) in the lower and middle atmosphere, reported in several studies,...
Identification of the causes of past climate change requires detailed knowledge of one of the most i...
International audienceAims. The solar activity in the past millennia can only be reconstructed from ...
The solar proxy 10Be, measured in natural archives, has previously been assumed to lag solar activit...
Understanding the transport path of the solar activity proxy Be-10 from source to archive is crucial...
International audienceBeryllium-10 in ice provides a valuable proxy of solar activity. However, comp...
Ice core concentrations of Be-10 are used as a proxy for solar activity, but they might be affected ...
Reconstruction of solar irradiance has only been possible for the Holocene so far. During the last d...
The atmospheric production rate of the cosmogenic isotope 10Be is modulated by the solar wind. Spect...
Beryllium 10 concentrations (Be-10(con)) were measured at annual resolution from varved sediment cor...
10Be concentrations measured in ice cores exhibit larger temporal variability than expected based on...
International audienceMore than 2,000 analyses of beryllium-10 (Be-10) and sulfate concentrations we...
In a recent paper (Usoskin et al., 2002a), we have reconstructed the concentration of the cosmogenic...
International audienceAll existing 10Be records from Greenland and Antarctica show increasing concen...
Solar cycle activity effects (SCAE) in the lower and middle atmosphere, reported in several studies,...
Identification of the causes of past climate change requires detailed knowledge of one of the most i...
International audienceAims. The solar activity in the past millennia can only be reconstructed from ...