Observations of thermospheric + exospheric Hα column emissions by the Wisconsin Hα Mapper (WHAM) Fabry-Perot (Kitt Peak, Arizona) over the 1997–2001 rise in solar cycle 23 show a statistically significant solar cyclical variation. The higher signal-to-noise WHAM observations corroborate suggestions of a solar cycle trend in the Hα emissions seen in Wisconsin observations over solar cycle 22. Here we compare WHAM 1997 and 2000–2001 winter solstice geocoronal Hα observations toward regions of the sky with low galactic emission. The observed variation in geocoronal hydrogen column emission intensities over the solar cycle is small compared with variations in hydrogen exobase densities. Higher Hα emissions are seen during solar maximum periods ...
Ground‐based hydrogen Balmer‐α observations from Northern midlatitudes span multiple solar cycles, f...
Hydrogen is a primary constituent of the geocorona and is a chemical byproduct of species below such...
Geocoronal H α and H β intensity measurements using the Wisconsin H α Mapper Fabry-Perot are used to...
Observations of thermospheric + exospheric Hα column emissions by the Wisconsin Hα Mapper (WHAM) Fab...
Understanding the influence of the solar cycle variation on the Earth\u27s upper atmosphere is impor...
The 11-year solar cycle is a dominant source of natural variability in the upper atmosphere, and its...
High precision observations during Solar Cycle 23 using the Wisconsin H‐alpha Mapper (WHAM) Fabry‐Pe...
Long term observations of geocoronal hydrogen offer potential to contribute to our understanding of ...
We will present observations of thermospheric exospheric hydrogen H-alpha emissions taken by the Wis...
Long term data sets are required to investigate sources of natural variability in the upper atmosphe...
Ground-based Fabry-Perot observations of the hydrogen Balmer-alpha emission have been used since the...
We will present geocoronal Hα intensity data taken over a four year time span during near solar mini...
The University of Wisconsin has observed geocoronal hydrogen Balmer-alpha emissions since the late 1...
We will discuss work in progress to better understand solar cyclic and climatic influences on hydrog...
Ground‐based hydrogen Balmer‐α observations from Northern midlatitudes span multiple solar cycles, f...
Hydrogen is a primary constituent of the geocorona and is a chemical byproduct of species below such...
Geocoronal H α and H β intensity measurements using the Wisconsin H α Mapper Fabry-Perot are used to...
Observations of thermospheric + exospheric Hα column emissions by the Wisconsin Hα Mapper (WHAM) Fab...
Understanding the influence of the solar cycle variation on the Earth\u27s upper atmosphere is impor...
The 11-year solar cycle is a dominant source of natural variability in the upper atmosphere, and its...
High precision observations during Solar Cycle 23 using the Wisconsin H‐alpha Mapper (WHAM) Fabry‐Pe...
Long term observations of geocoronal hydrogen offer potential to contribute to our understanding of ...
We will present observations of thermospheric exospheric hydrogen H-alpha emissions taken by the Wis...
Long term data sets are required to investigate sources of natural variability in the upper atmosphe...
Ground-based Fabry-Perot observations of the hydrogen Balmer-alpha emission have been used since the...
We will present geocoronal Hα intensity data taken over a four year time span during near solar mini...
The University of Wisconsin has observed geocoronal hydrogen Balmer-alpha emissions since the late 1...
We will discuss work in progress to better understand solar cyclic and climatic influences on hydrog...
Ground‐based hydrogen Balmer‐α observations from Northern midlatitudes span multiple solar cycles, f...
Hydrogen is a primary constituent of the geocorona and is a chemical byproduct of species below such...
Geocoronal H α and H β intensity measurements using the Wisconsin H α Mapper Fabry-Perot are used to...