The Saturation of Dayside Magnetosphere Erosion

Physics

Scientific paper

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2700 Magnetospheric Physics

Scientific paper

We carry out a statistical investigation relating the depression of the geostationary magnetic field near noon to the strength of the southward component of the IMF (Bz). We use measurements made by GOES, WIND, ACE and ground-based magnetograms. The period studied is 1996--2003. Events have been selected during intervals with (1) a steady dynamic pressure, Pdyn; (2) a steady and negative IMF Bz; (3) when one of the GOES spacecraft was within 2 hours of local noon; and (4) during substorm growth phase (as ascertained by readings from nightside ground magnetometers). The investigation starts with a correction of raw values of the total geostationary field, Btot, for the compression due to Pdyn. To do this, we chose a number of ``reference" days encompassing a wide range of Pdyn values when the IMF was strongly northward (clock angle < 45o), and fitted Btot to the functional form Btot = a + b Pdyn1/2. We then fit the corrected Δ Btot values as a function of Bz. This work extends the investigation of Mühlbachler et al., 2004 by a set of events with extremly large and negative Bz in the range of [0,-52]nT. Thus, we find that saturation of erosion occurs for Bz in the range -12 to -16 nT. We fit the data in several ways and find Δ Btot = -27.76 + 26.1 exp(0.012 Bz) to lie closest to our set of data.

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