Variable Earth's Rotation Speed in the 14th to 16th Centuries: New {Delta}T Constraints from Chinese Eclipse Records
Pith reviewed 2026-05-10 18:40 UTC · model grok-4.3
The pith
Chinese eclipse records from Ming local treatises yield tighter bounds on Earth's rotation changes from 1361 to 1575.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
Using eclipse records that explicitly mentioned totality from (quasi-)contemporaneous local treatises compiled during the Ming Dynasty, and employing the NASA JPL DE 441 ephemeris, we revised the ΔT constraint in 1361 to -408 s ≤ ΔT ≤ 601 s and set new constraints of 277 s ≤ ΔT ≤ 890 s in 1514, -328 s ≤ ΔT ≤ 332 s in 1542, and -1762 s ≤ ΔT ≤ 1091 s in 1575. Overall, our ΔT constraints generally tighten the ΔT variations more than what prior fits produced for their ΔT spline curve, requiring downward modification around 1361 and upward modification around 1542, while suggesting that the ΔT decrease between 1514 and 1567 was slightly steeper than previously considered.
What carries the argument
ΔT constraints obtained by matching reported totality times and locations of historical solar eclipses against modern orbital predictions, which quantify the accumulated difference between Terrestrial Time and Universal Time.
Load-bearing premise
The local treatises accurately recorded the dates, locations, and occurrence of totality for the eclipses without significant errors that would prevent direct comparison to modern predictions.
What would settle it
Re-examination of the original local treatises revealing systematic errors in recorded eclipse dates, locations, or totality claims that shift the calculated ΔT bounds outside the reported ranges.
Figures
read the original abstract
Total solar eclipses are not only astronomical spectacles but also great astrophysical laboratories. Their historical records are particularly helpful for assessing the past variability of the Earth's rotation speed. Chinese records played a key role for such analyses. However, Chinese eclipse records from the M\'ing period have not been used for {\Delta}T reconstructions, partially because most of the contemporaneous eclipse reports are found not in official histories but in local treatises. This study examines eclipse records in the (quasi-)contemporaneous local treatises, concentrating on what explicitly mentioned eclipse totality on the day of a total solar eclipse and what were compiled during the M\'ing Dynasty. On their basis, our study revised the {\Delta}T constraint in 1361 to -408 s =< {\Delta}T =< 601 s and set new {\Delta}T constraints of 277 s =< {\Delta}T =< 890 s in 1514, -328 s =< {\Delta}T =< 332 s in 1542, and -1762 s =< {\Delta}T =< 1091 s in 1575, respectively. We also revised most of the existing {\Delta}T constraints in the 14th to 16th centuries, using the ephemeris data of the NASA JPL DE 441. Overall, our {\Delta}T constraints generally tighten the {\Delta}T variations more than what M+21 fit for their {\Delta}T spline curve, requiring downward modification and upward modifications for the {\Delta}T reconstructions around 1361 and 1542, respectively. Our results suggest that the {\Delta}T decrease between 1514 and 1567 was slightly steeper than previously considered.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript derives revised and new constraints on the historical ΔT parameter (terrestrial time minus universal time) for the 14th–16th centuries by analyzing Chinese total solar eclipse records from (quasi-)contemporaneous Ming-dynasty local treatises that explicitly mention totality. Using the JPL DE441 ephemeris, it updates the 1361 bound to −408 s ≤ ΔT ≤ 601 s, introduces new bounds for 1514 (277 s ≤ ΔT ≤ 890 s), 1542 (−328 s ≤ ΔT ≤ 332 s), and 1575 (−1762 s ≤ ΔT ≤ 1091 s), revises most existing 14th–16th century constraints, and argues that these tighten ΔT variations relative to the M+21 spline fit, implying a steeper decrease between 1514 and 1567.
Significance. If the record interpretations hold, the tighter ΔT intervals would refine models of Earth's rotation variability in the late medieval period, with downstream value for geophysical studies of tidal friction and core-mantle coupling. The use of previously under-exploited local treatises expands the historical dataset beyond official histories, which is a constructive contribution provided the selection and error-handling steps are made fully transparent.
major comments (2)
- [record selection and results] The revised ΔT intervals (e.g., −408 s ≤ ΔT ≤ 601 s for 1361 and 277 s ≤ ΔT ≤ 890 s for 1514) are obtained by requiring that the DE441 umbral path passes over the reported observer location when the treatise states totality. This mapping is load-bearing for all new and revised bounds, yet the manuscript provides no quantitative assessment of possible dating, location, or totality-reporting errors in the local treatises, nor any cross-check against independent Ming sources (see the record-selection and results paragraphs).
- [comparison with M+21] The claim that the new constraints require downward modification around 1361 and upward modification around 1542 relative to the M+21 spline, and that the 1514–1567 decrease was slightly steeper, rests on direct comparison of the new intervals to the prior spline. Without an explicit overlay of the updated spline or a table quantifying the change in spline coefficients or knot values, the magnitude of the suggested revision cannot be evaluated.
minor comments (2)
- [references] The abstract and text repeatedly use the placeholder “M+21” without a full bibliographic entry; the reference list should supply the complete citation (presumably Morrison et al. 2021 or equivalent).
- [abstract and results] Notation for the inequality bounds is inconsistent (sometimes “=<”, sometimes “≤”); standardize to a single symbol throughout.
Simulated Author's Rebuttal
We thank the referee for their thorough review and valuable suggestions. We address the major comments below and will incorporate revisions to enhance the clarity and robustness of our analysis.
read point-by-point responses
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Referee: The revised ΔT intervals (e.g., −408 s ≤ ΔT ≤ 601 s for 1361 and 277 s ≤ ΔT ≤ 890 s for 1514) are obtained by requiring that the DE441 umbral path passes over the reported observer location when the treatise states totality. This mapping is load-bearing for all new and revised bounds, yet the manuscript provides no quantitative assessment of possible dating, location, or totality-reporting errors in the local treatises, nor any cross-check against independent Ming sources (see the record-selection and results paragraphs).
Authors: We agree that a quantitative assessment of potential errors would strengthen the manuscript. The selection of records was based on explicit mentions of totality in (quasi-)contemporaneous local treatises compiled during the Ming Dynasty, which we believe minimizes some uncertainties. However, in the revised version, we will add a new subsection under Methods or Results detailing possible sources of error in dating, location identification, and the interpretation of totality reports, including any available historical context for uncertainty estimates. We will also perform and report cross-checks against any independent Ming sources that mention the same events, noting limitations where such sources are unavailable or less detailed. revision: yes
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Referee: The claim that the new constraints require downward modification around 1361 and upward modification around 1542 relative to the M+21 spline, and that the 1514–1567 decrease was slightly steeper, rests on direct comparison of the new intervals to the prior spline. Without an explicit overlay of the updated spline or a table quantifying the change in spline coefficients or knot values, the magnitude of the suggested revision cannot be evaluated.
Authors: We concur that an explicit comparison would better illustrate the implications of our new constraints. In the revised manuscript, we will add a figure showing the M+21 spline with our new ΔT bounds overlaid, and include a table that quantifies the differences at the relevant epochs (e.g., around 1361, 1514, 1542, 1567) and the change in the slope of the ΔT curve between 1514 and 1567. This will provide a clear, quantitative evaluation of how our results modify the previous fit. revision: yes
Circularity Check
No circularity: ΔT bounds from direct ephemeris comparison
full rationale
The paper's core derivation compares reported eclipse totality at specific locations and dates against predictions from the independent external ephemeris DE441. This produces numerical ΔT intervals (e.g., -408 s ≤ ΔT ≤ 601 s for 1361) without fitting any parameters to the historical data and then reusing those fits as predictions. No self-citations justify uniqueness theorems, ansatzes, or load-bearing premises; M+21 is cited only for prior spline context. The chain is self-contained against external benchmarks (ephemeris + records) and does not reduce to its inputs by construction.
Axiom & Free-Parameter Ledger
axioms (2)
- domain assumption The selected local treatises provide accurate, contemporaneous descriptions of eclipse totality at the reported locations and dates.
- domain assumption NASA JPL DE 441 ephemeris provides sufficiently accurate Sun-Moon positions for the 14th-16th centuries to compute expected eclipse circumstances.
Reference graph
Works this paper leans on
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[3]
Introduction Total solar eclipses have served human beings not only as one of the greatest astronomical spectacles, but also as one of the unique astrophysical laboratories (Orchiston et al., 2015; Littmann and Espenak, 2017; Pasachoff, 2017). Their long-term records have been used for multiple scientific measurements such as those for the solar coronal s...
work page 2015
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[4]
and solar diameters (Fiala et al., 1994; Rozelot and Damiani, 2012). These records have also served as vital references to assessing and reconstructing the long-term variability of Earth’s rotation speed before the 1620s (Stephenson, 1997, hereafter S97; Sôma and Tanikawa, 2015; Orchiston et al., 2015; Stephenson et al., 2016, hereafter SMH16; Morrison et...
work page 1994
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[5]
(2018) in the context of the ΔT reconstructions
have been of particular importance and have been intensively studied by Stephenson et al. (2018) in the context of the ΔT reconstructions. In contrast, Chinese eclipse records from the Míng (明) Dynasty (1368 –
work page 2018
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[7]
and our methodology (Section 3), we develop case studies on the individual eclipses in 1361 (Section 4), 1514 (Section 5), 1542 (Section 6), and 1575 (Section 7), where Chinese local treatises explicitly mention the local total obscurations. We then revise most of the ΔT constraints that M+21 used for their ΔT reconstructions in the 14th to 16th centuries...
work page 2014
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[9]
We agree with this interpretation, as this local treatise was compiled in Wànlì 24th year (≈
Beijing Observatory (1988) omitted the 1542 entries and included only the 1575 entries for a good reason. We agree with this interpretation, as this local treatise was compiled in Wànlì 24th year (≈
work page 1988
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[10]
and the author has a higher probability of having an experience or a direct hearsay of the 1575 eclipse rather than the 1542 eclipse. Owing to their motivations, these local treatises generally describe the local events that occurred locally in the administrative units to which their contents were dedicated. S97 associated Sōngjiāngfǔzhì (松江府志) twice with...
work page 1958
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[12]
Materials and Methods In order to satisfy the said purpose, we first picked up the dates for total solar eclipses that were viewed in China during the reigns of the Yuán and Míng Dynasties, using the NASA Five Millennium Catalog of Solar Eclipses (Espenak and Meeus, 2009). We then compared their dates to the union catalog of Chinese astronomical records (...
work page 2009
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[23]
For the 1330 ΔT constraint, M+21 used a Zbraslav report of a partial eclipse on 16 July 1330, rejecting other records of Tüngedaer Schloß and Constantinople. The source report is acquired from Chronicon Aulae Regiae, by hand of local Cistercian abbots (Antonín, 2019). This monastery was located in the old town area of Zbraslav (N49°58.5' E014°23.5'). In o...
work page 2019
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[25]
For the 1406 ΔT constraint, M+21 used a Bordeaux report and a Liege report for a total solar eclipse on 16 June 1406 and rejected a Hamburg report that S97 and Tanikawa et al. (2023, hereafter T+23) used. However, M+21 located Hamburg to N53°33', E007°38', near modern Wittmundhafen Air Base of Lower Saxony. This is some 160 km westward from Hamburg (N53°3...
work page 2023
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[27]
SMH16 and M+21 commonly use this eclipse for one of their ΔT constraints. In order to locate Augsburg (N48°22', E010°54') and Karlštejn (N49°56', E014°11') in the totality path, we need to set ΔT constraints of −995 s ≤ ΔT ≤ 575 s and 413 s ≤ ΔT ≤ 2034 s, respectively. In combination, we need to set a ΔT constraint of 413 s ≤ ΔT ≤ 575 s in 1433 to satisfy...
work page 2034
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[29]
In order to locate Bourges (N47°05', E002°24') and Fribourg (N46°48', E007°10') in the totality path, we need to set ΔT constraints of −1867 s ≤ ΔT ≤ 497 s and −227 s ≤ ΔT ≤ 1955 s, respectively. In combination, we need to set a ΔT constraint of −227 s ≤ ΔT ≤ 497 s in 1485 to satisfy these reports. This result slightly improves M+21’s existing ΔT constrai...
work page 1955
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[30]
into M+21’s existing ΔT constraints and ΔT spline curve, revising one ΔT constraint (1361) and adding three new ΔT constraints (1514, 1542, and 1575). Our revision of the 1361 eclipse reports requires us to either revise M+21's ΔT spline curve upward (from ΔT = 557 s to 602 s ≤ ΔT ≤ 1864 s) or change the interpretation for the local eclipse visibility fro...
work page 2020
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[32]
Rediscovery of Citizen Science Culture in the Regions and Today
In combination, these data allow us to tentatively set the actual ΔT values in 1542 as 277 s ≤ ΔT ≤ 332 s. These constraints are compared with the ΔT constraint of 145 s ≤ ΔT ≤ 165 s in 1567 (Stephenson et al., 1997; M+21). This study allows us to detect short-term ΔT fluctuations that SMH16 and M+21’s ΔT spline curves have missed so far. It is desired to...
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[33]
DOI: 10.1051/swsc/2020035 Hayakawa, H., Murata, K., Sôma, M. 2022, The Variable Earth's Rotation in the 4th–7th Centuries: New ΔT Constraints from Byzantine Eclipse Records, Publications of the Astronomical Society of the Pacific, 134, 094401. DOI: 10.1088/1538-3873/ac6b56 Hayakawa, H., Murata, K., Owens, M. J., Lockwood, M. 2024, Analyses for graphical r...
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DOI: 10.3847/1538-3881/abd414 (P+21) Pasachoff, J. M. 2017, Heliophysics at Total Solar Eclipses, Nature Astronomy, 1,
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F., Chen, J., Dehant, V., Rosat, S., Zhu, P
DOI: 10.1038/s41550-017-0190 Rekier, J., Chao, B. F., Chen, J., Dehant, V., Rosat, S., Zhu, P. 2022, Earth's Rotation: Observations and Relation to Deep Interior, Riley, P., Lionello, R., Linker, J. A., et al. 2015, Inferring the Structure of the Solar Corona and Hayakawa, Sôma, and Li (2026) Monthly Notices of the Royal Astronomical Society, DOI: 10.1093...
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DOI: 10.1088/0004-637X/802/2/105 Rozelot, J. P., Damiani, C. 2012, Rights and Wrongs of the Temporal Solar Radius Variability, The European Physical Journal H, 37, 709-743. DOI: 10.1140/epjh/e2012-20030-4 Stephenson, F. R. 1997, Historical Eclipses and Earth's Rotation, Cambridge, Cambridge University Press (S97) Stephenson, F. R., Morrison, L. V., Hohenk...
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Their copies are also found elsewhere
DOI: 10.1007/s00190-021-01513-9 Appendix: Source Documents They are shown in their original languages with a reference ID in the National Central Library of Hayakawa, Sôma, and Li (2026) Monthly Notices of the Royal Astronomical Society, DOI: 10.1093/mnras/stag656 26 Taipei (NCL). Their copies are also found elsewhere. See Kanseki Database5 to locate thei...
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