EGU21-10704
https://doi.org/10.5194/egusphere-egu21-10704
EGU General Assembly 2021
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Quantifying the lobe reconnection rate during dominant IMF By periods

Jone Peter Reistad1, Karl Magnus Laundal1, Anders Ohma1, Nikolai Østgaard1, Spencer Hatch1, Stein Haaland1,2, and Evan Thomas3
Jone Peter Reistad et al.
  • 1University of Bergen, Birkeland Centre for Space Science, Department of Physics and Technology, Bergen, Norway (jone.reistad@uib.no)
  • 2Max-Planck Institute for Solar System Research, Göttingen, Germany
  • 3Thayer School of Engineering, Dartmouth College, Hanover, NH, USA

Lobe reconnection is usually considered to play an important role in geospace dynamics only when the Interplanetary Magnetic Field (IMF) is mainly northward. This is because the most common signature of lobe reconnection is the strong sunward convection in the polar cap ionosphere observed during these conditions. During more typical conditions, when the IMF is mainly in a dawn-dusk direction, plasma flows initiated by dayside as well as lobe reconnection map to high latitude ionospheric locations in close proximity to each other. This has been emphasized in the literature earlier, mainly on a conceptual level, but quantifying the relative importance of lobe reconnection to the observed ionospheric convection is highly challenging during these IMF By dominated conditions, since one has to identify and distinguish these regions. By normalizing the ionospheric convection (observed by SuperDARN) to the polar cap boundary (inferred from simultaneous AMPERE observations), we are able to do this separation, allowing us to quantify the relative contribution of both lobe reconnection and dayside/nightisde reconnection to the ionospheric convection pattern. Using this segmentation technique we can get new quantitative insights into the importance of the various mechanisms that affect the lobe reconnection rate. In this presentation we will describe the technique and show results of analysis of periods when the IMF is mainly in the dawn-dusk direction. Our quantification of the average lobe reconnection rate during various conditions yields quantitative knowledge of the importance of the lobe reconnection process, which can act independently in the two hemispheres. We will specifically constrain the influence from parameters such as the dipole tilt angle and the product of IMF transverse component and solar wind velocity.

How to cite: Reistad, J. P., Laundal, K. M., Ohma, A., Østgaard, N., Hatch, S., Haaland, S., and Thomas, E.: Quantifying the lobe reconnection rate during dominant IMF By periods, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-10704, https://doi.org/10.5194/egusphere-egu21-10704, 2021.

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