Trends in the upper atmosphere, together with the global warming of the lower atmosphere, are part of the global change of the Earth system. In the present work, which is focused in the upper atmosphere, long-term variations of the critical frequency of the ionospheric F2 layer, foF2, are studied in terms of the following possible causes: (1) longterm variations of the solar EUV radiation shown by the solar cycle length (SCL), (2) long-term variations in geomagnetic activity measured by the aa index, (3) the increasing greenhouse gases concentration in the lower atmosphere which would be producing a temperature decrease in the upper atmosphere, and (4) the Earth’s main magnetic field secular variation, which implies changes in the dip angle...
Geomagnetic activities frequently occur in varying degrees. Strong geomagnetic activities, which hav...
The trend of the peak height of the ionospheric F2 layer, hmF2, during three solar cycles (1957?1986...
A new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly foF2 and M(3000)...
The Earth's magnetic field presents long-term variations with changes in strength and orientation. P...
<p>The lower and middle atmosphere present long-term variations in temperature and other parameters ...
The lower and middle atmosphere present long-term variations in temperatureand other parameters link...
The first part of the paper is directed to the investigation of the practical importance of possible...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
The first part of the paper is directed to the investigation of the practical importance of possible...
It is well known that the Earth magnetic field, as well as geomagnetic activity, presents long-term ...
Geomagnetic activities frequently occur in varying degrees. Strong geomagnetic activities, which hav...
Results of various authors on long-term trends in foF2, which is equivalent to the maximum electron ...
Geomagnetic activities frequently occur in varying degrees. Strong geomagnetic activities, which hav...
The trend of the peak height of the ionospheric F2 layer, hmF2, during three solar cycles (1957?1986...
A new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly foF2 and M(3000)...
The Earth's magnetic field presents long-term variations with changes in strength and orientation. P...
<p>The lower and middle atmosphere present long-term variations in temperature and other parameters ...
The lower and middle atmosphere present long-term variations in temperatureand other parameters link...
The first part of the paper is directed to the investigation of the practical importance of possible...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
Based on an analysis of the midday data of the midlatitude ionospheric stations in the Northern Hemi...
The first part of the paper is directed to the investigation of the practical importance of possible...
It is well known that the Earth magnetic field, as well as geomagnetic activity, presents long-term ...
Geomagnetic activities frequently occur in varying degrees. Strong geomagnetic activities, which hav...
Results of various authors on long-term trends in foF2, which is equivalent to the maximum electron ...
Geomagnetic activities frequently occur in varying degrees. Strong geomagnetic activities, which hav...
The trend of the peak height of the ionospheric F2 layer, hmF2, during three solar cycles (1957?1986...
A new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly foF2 and M(3000)...