Masao Nakada

Profile

Present Address:

Department of Earth and Planetary Sciences, Faculty of Science, Kyushu University 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan
E-mail: mnakada [at] geo.kyushu-u.ac.jp

Education Background:

[1] 03/1976: B.Sc. in Geophysics, University of Tokyo
[2] 03/1978: M.Sc. in Geophysics, University of Tokyo
[3] 03/1983: D.Sc. in Geophysics, University of Tokyo

Positions Held:

[1] 04/1983-05/1984: JSPS Postdoctoral Fellow, Ocean Research Institute, University of Tokyo
[2] 06/1984-07/1988: Research Fellow, Research School of Earth Sciences, Australian National University
[3] 08/1988-03/1994: Associate Professor, Kumamoto University
[4] 04/1994-07/1996: Associate Professor, Kyushu University
[5] 08/1996-present: Professor, Kyushu University

Recent Research Topics

Earth’s viscosity structure
Recent sea level rise and vertical tectonic movement of Japanese Islands
Decay of Chandler wobble and viscosity of D” layer

Earth’s viscosity structure

Viscosity structure of Earth’s mantle is a crucial quantity in discussing mantle dynamics. One of the methods for inferring viscosity structure is to use the observed relative sea level (RSL) variations for glacial isostatic adjustment (GIA) process due to the last deglaciation during the past ~20 kyr (kilo-year). On the other hand, the rotational variations due to the GIA processes are degree-two response of the Earth, and therefore have been used to infer the lower mantle viscosity. In particular, the rate of change of degree-two harmonics of Earth’s geopotential, J2/dt (J2-dot), provides an important constraint on the lower mantle viscosity. However, the observationally derived J2-dot is affected by recent melting of glaciers and the Greenland and Antarctic ice sheets, and therefore we have to extract the recent melting component from the observation to estimate the GIA-induced J2-dot available for inferring the viscosity structure. Thus, Nakada et al. (2015) estimated the recent melting component using the data taken from the IPCC 2013 Report and obtained the GIA-induced J2-dot based on the observationally derived J2-dot.
GIA-induced J2-dot is also highly sensitive to the Late Pleistocene melting histories of the Northern and Southern hemisphere ice sheets, particularly, to the meltwater volume since the Last Glacial Maximum (~ 21 kyr BP) characterized by globally averaged (eustatic) sea level (ESL) rise. For example, Peltier’s group (Toronto University) support an ESL component of ~120 m, and Lambeck’s group (Australian National University) support the component of ~130 m.
Recently, we have examined the GIA-induce J2-dot and LGM sea level changes at Barbados and Bonaparte Gulf, Australia, to infer the viscosity structure and the ESL component. These results indicate the effective lower mantle viscosity of(5-10)x10^22 Pa s, upper mantle viscosity of (1-3)x10^20 Pa s and the preferred ESL component of ~130 m. Please see the following papers:

  1. Nakada, M., Okuno, J. and Yokoyama, Y., 2015. Total meltwater volume since the Last Glacial Maximum and viscosity structure of Earth’s mantle inferred from relative sea level changes at Barbados and Bonaparte Gulf and GIA-induced J2-dot, Geophysical Journal International (in press).
  2. Nakada, M., Okuno, J., Lambeck, K. and Purcell, A., 2015. Viscosity structure of Earth’s mantle inferred from rotational variations due to GIA process and recent melting events, Geophysical Journal International, vol. 202, 976-992.
  3. Nakada, M. and Okuno, J., 2013. GIA-related rotational variations for the Earth with low-viscosity D” layer, Geophysical Journal International, vol. 195, 725-739.

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©Masao Nakada