Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/8495
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dc.contributor.authorKharayat, Hema-
dc.contributor.authorSingh, J-
dc.contributor.authorPriyal, M-
dc.contributor.authorRavindra, B-
dc.date.accessioned2024-06-28T08:49:49Z-
dc.date.available2024-06-28T08:49:49Z-
dc.date.issued2024-06-20-
dc.identifier.citationThe Astrophysical Journal, Vol. 968, No. 2, 53en_US
dc.identifier.issn1538-4357-
dc.identifier.urihttp://hdl.handle.net/2248/8495-
dc.descriptionOpen Access.en_US
dc.descriptionOriginal content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.-
dc.description.abstractDifferential rotation is one of the basic characteristics of the Sun, and it plays an important role in generating the magnetic fields and its activities. We investigated rotation rate using chromospheric features such as plages, enhanced network (EN), active network (AN), and quiet network (QN) separately (for the first time). The digitized Ca-K images from Kodaikanal Observatory for 1907–1996 are used to study rotation over 0°–80° latitudes at an interval of 10°. We find that plages and all types of networks exhibit the differential rotation of the chromosphere. Furthermore, the rotation rate shows a decreasing pattern as one move from the equator to the higher polar latitudes for all the features used in the study. At the equator the rotation rate (rotation period) is obtained to be ∼13.98° day−1 (25.74 days), ∼13.91° day−1 (25.88 days), ∼13.99° day−1 (25.74 days), and ∼14.11° day−1 (25.51 days) for plage, EN, AN, and QN areas, respectively. By analyzing how the area of chromospheric features varies over time, we can effectively map the Sun’s rotation rate at all latitudes, including the polar regions. Interestingly, both plages and small-scale networks exhibit a similar differential rotation rate. This suggests these features likely rooted at the same layer below the visible surface of the Sun. Therefore, the long-term Ca-K data is very useful for studying the solar rotation rate at all latitudes including the polar regions.en_US
dc.language.isoenen_US
dc.publisherAmerican Astronomical Societyen_US
dc.relation.urihttps://doi.org/10.3847/1538-4357/ad4992-
dc.rights© 2024. The Author(s)-
dc.subjectSolar chromosphereen_US
dc.subjectPlagesen_US
dc.subjectSolar rotationen_US
dc.subjectSolar differential rotationen_US
dc.titleEquator to Pole Solar Chromospheric Differential Rotation Using Ca-K Features Derived from Kodaikanal Dataen_US
dc.typeArticleen_US
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