• 検索結果がありません。

昭和基地の平均海水位の経年変動再考 渋谷

N/A
N/A
Protected

Academic year: 2021

シェア "昭和基地の平均海水位の経年変動再考 渋谷"

Copied!
2
0
0

読み込み中.... (全文を見る)

全文

(1)

昭和基地の平均海水位の経年変動再考

渋谷 和雄1,2、早河 秀章1, 3

1国立極地研究所

2

特任教授

3

56

次隊員

Decadal Variation of Mean Sea Level at Syowa Station Revisited

Kazuo Shibuya

1

, Hideaki Hayakawa

1

1

National Institute of Polar Research (NIPR)

2

Emeritus Professor,

3

JARE-56 Member

Analyses of tidal observations at Nisino-ura-cove of Syowa Station were made intermittently by several authors. Hither-to the applied data periods were e.g. 8 years (1981-1998) by Odamaki et al.

(1991), 15 years (1981-1996) by Yaguchi et al. (2001), and 20 year (1980 - 2000) by Tateoka et al.

(2008). The obtained trends were about -1.0 cm/yr ~ -1.4 cm/yr; always indicating negative sign of sea level falling.

In this study, we expanded the data period to 24 years (1979 - 2003), using all available JARE Data Reports Oceanography Series, and unified to the reference level at 28 January 1979 below the BM No. 1040. Figure 1 illustrates the plot of monthly mean sea level (solid circles) and annual mean sea level (solid squares). Previously it was interpreted that systematic decrease of annual variation must be related with sensitivity change of the sensor, but recovery of Sa amplitude after 1994 and change of trend to positive for the overlapped long-period (probably 30 years) S

0

variation strongly supports that this decadal variation is related with climatology-driven phenomenon.

This decadal variations are not correlated with AAO nor ECCO OBP height variation, and the cause of this variation is not found at present. We discuss here some comparison with the ellipsoidal height variation of SYOG, secular gravity change at the IAGBN#0417 point, and long-period seal level changes at Mawson and Faraday-Vernatsky stations.

References

Odamaki, M., Michida, Y., Noguchi, I., Iwanaga, Y., Ikeda, S., Iwamoto, K., 1991. Mean sea-level observed at Syowa Station, East Antarctica. Proc. NIPR Symp. Antarct. Geosci., 5, 20-28.

Tateoka, A., Michida, Y., Kinoshita, H., Namiki, M., Odamaki, M., 2008. The seasonal change of sea level at Syowa Station, Antarctica for the period of 1981-2000.

Yaguchi, A., and others from GSI, JHD and NIPR, 2000. Report of current activities of Japan for

1998-2000 to SCAR WG-GGI.

(2)

Fig. 1. Variation of monthly mean sea level (solid circle) and annual mean

sea level (solid squares) at Syowa Station.

参照

関連したドキュメント

Standard domino tableaux have already been considered by many authors [33], [6], [34], [8], [1], but, to the best of our knowledge, the expression of the

Rev. Localization in bundles of uniform spaces. Colom- biana Mat. Representation of rings by sections. Representation of algebras by continuous sections.. Categories for the

Notice that for the adjoint pairs in corollary 1.6.11 conditions (a) and (b) hold for all colimit cylinders as in (1.93), since (F ? , F ∗ ) is an equipment homomorphism in each

It was shown in [ALM] that the parameter space of general analytic families of unimodal maps (with negative Schwarzian derivative) can be related to the parameter space of

Instead an elementary random occurrence will be denoted by the variable (though unpredictable) element x of the (now Cartesian) sample space, and a general random variable will

Figure 12 shows that specific loss R 1 decrease sharply for small values of ω but decrease with small variation as increases further for LS and GL theories of microstretch

In this paper we prove the existence and uniqueness of local and global solutions of a nonlocal Cauchy problem for a class of integrodifferential equation1. The method of semigroups

Within the family of isosceles 4-simplices with an equifacetal base, the degree of freedom in constructing an equiareal, equiradial, but non-equifacetal simplex is embodied in