2019
DOI: 10.1029/2019sw002204
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Near‐Earth Solar Wind Forecasting Using Corotation From L5: The Error Introduced By Heliographic Latitude Offset

Abstract: Routine in situ solar wind observations from L5, located 60° behind Earth in its orbit, would provide a valuable input to space weather forecasting. One way to utilize such observations is to assume that the solar wind is in perfect steady state over the 4.5 days it takes the Sun to rotate 60°, and thus, near‐Earth solar wind in 4.5 days time would be identical to that at L5 today. This corotation approximation is most valid at solar minimum when the solar wind is slowly evolving. Using STEREO data, it has bee… Show more

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Cited by 20 publications
(33 citation statements)
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“…30 gives the photospheric magnetic field configuration on the Sun using magnetic field extrapolations from GONG data marking open and closed field lines. With such inevitable differences in the latitude between the measuring spacecraft, rather large uncertainties in the 1 AU measured speed of a particular coronal hole are obtained (see Hofmeister et al 2018;Owens et al 2019). Recent studies suggest that solar wind forecasting based on persistence models may work best when using a combination of spacecraft located behind Earth (L5 position or STEREO data from time-varying spacecraft position) and empirical or numerical solar wind modeling (see e.g., Opitz et al 2010;Temmer et al 2018;Owens et al 2019;Bailey et al 2020).…”
Section: Background Solar Windmentioning
confidence: 99%
“…30 gives the photospheric magnetic field configuration on the Sun using magnetic field extrapolations from GONG data marking open and closed field lines. With such inevitable differences in the latitude between the measuring spacecraft, rather large uncertainties in the 1 AU measured speed of a particular coronal hole are obtained (see Hofmeister et al 2018;Owens et al 2019). Recent studies suggest that solar wind forecasting based on persistence models may work best when using a combination of spacecraft located behind Earth (L5 position or STEREO data from time-varying spacecraft position) and empirical or numerical solar wind modeling (see e.g., Opitz et al 2010;Temmer et al 2018;Owens et al 2019;Bailey et al 2020).…”
Section: Background Solar Windmentioning
confidence: 99%
“…Recently, we used magnetogram-constrained simulations of the solar wind to estimate the difference in solar wind speed encountered at Earth and the L5 position, 60°behind Earth in its orbit, owing entirely to the small time-varying difference in latitude (Owens et al, 2019a, hereafter "Paper 1"). While the latitudinal difference is small, varying from 0°to approximately 7°over the year, it can lead to sampling significantly different solar wind streams at the two locations, even under the perfectly steady-state approximation.…”
Section: Introductionmentioning
confidence: 99%
“…L5 reaches a maximum |Δθ| of around 5° with Earth (at times close to the summer and winter solstices), meaning that the latitudinal variation can be largely disregarded. Owens et al (2019) showed that there is a time-of-year variation in the modeled impact of |Δθ| on MAE. This is not investigated here due to data limitations.…”
Section: Discussionmentioning
confidence: 99%