Comment on “Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply” | Zendy

Peter Huybers | Zendy; C. H. Langmuir | Zendy; Richard F. Katz | Zendy; David Ferguson | Zendy; Cristian Proistosescu | Zendy; S. M. Carbotte | Zendy

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Comment on “Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply”

Author(s) -

Peter Huybers,

C. H. Langmuir,

Richard F. Katz,

David Ferguson,

Cristian Proistosescu,

S. M. Carbotte

Publication year - 2016

Publication title -

science

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 12.556

H-Index - 1186

eISSN - 1095-9203

pISSN - 0036-8075

DOI - 10.1126/science.aae0451

Subject(s) - bathymetry , seafloor spreading , ridge , geology , oceanography , mid ocean ridge , forcing (mathematics) , sea level , climatology , sensitivity (control systems) , environmental science , paleontology , electronic engineering , engineering

Olive et al. (Reports, 16 October 2015, p. 310) argue that order 10% fluctuations in melt supply do not produce appreciable changes in ocean ridge bathymetry on time scales less than 105 years, and thus cannot reflect sea-level forcing. Spectral analysis of bathymetry in a region they highlight as being fault controlled also shows strong evidence for a signal from sea level variation

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