Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay

Zhang Keqi; Jin Qingxiang; Wang Baocan

doi:10.1007/BF02850637

Your Location：

Home >

Browse articles >

Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay

OriginalPaper | Updated：2023-05-16

- Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay
- Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay
- 海洋湖沼学报（英文） 1993年11卷第4期页码：321-332
- Affiliations：
  
  Institute of Estuarine and Coastal Research
- Author bio：
- Funds：
- DOI：10.1007/BF02850637
  中图分类号：
- 纸质出版：1993
- Accepted：
Scan QR Code
Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay[J]. 海洋湖沼学报（英文）, 1993,11(4):321-332.

Keqi, Z., Qingxiang, J. & Baocan, W. Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay., Chin. J. Ocean. Limnol. 11, 321–332 (1993). https://doi.org/10.1007/BF02850637
Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay[J]. 海洋湖沼学报（英文）, 1993,11(4):321-332. DOI： 10.1007/BF02850637.

Keqi, Z., Qingxiang, J. & Baocan, W. Seasonal changes of the tidal flat from Jinhuigang to Caojing along the north bank of Hangzhou Bay., Chin. J. Ocean. Limnol. 11, 321–332 (1993). https://doi.org/10.1007/BF02850637 DOI：

摘要

Abstract

This paper deals with the seasonal changes of the tidal flat along the north bank of Hangzhou Bay. Analysis of a one year set of weekly measured tidal flat profiles from Jinhuigang to Caojing shows that the tidal flat on the north bank of Hangzhou Bay accretes during winter and erodes during summer. To identify the characteristic patterns of the tidal flat spatio-temporal variations

Empirical Orthogonal Function (EOF) is applied on the tidal flat profile data. The results show that most of the variations of the tidal flat profiles can be represented by three eigenfunctions corresponding to the three largest eigenvalues. The first eigenfunction represents the long-term variation of the tidal flat over a year

the second eigenfunction represents the seasonal changes of the tidal flat resulting from the seasonal variations in wave regime

the third eigenfunction indicates sediment exchanges between different parts of the tidal flat associated with the variations of sea level.

关键词

Keywords

references

Anderson, F. and Blanck, I., 1980. A temporal and spatial study of mudflat erosion and derosition.J. Sed. Petrology 51(3): 729–736.

Aranuvachapun, S. and Johnson, A. J., 1979. Beach profiles at Gorleston and Great Yarmouth.Coastal Eng. 2: 201–213.

Aubrey, D. G., 1979. Seasonal patterns of onshore-offshore sediment movement.J. Geophys. Res. 84: 6347–6354.

Aubrey, D. G., 1980. The statistical prediction of beach changes in southern California.J. Geophys. Res. 85(C6): 3264–3276.

Carling, P. A., 1982. Temporal and spatial variation in intertidal sedimentation rates.Sedimentology 29: 17–23.

Clarke, D. J. and Eliot, I. G., 1988. Low-frequency variation in the seasonal intensity of coastal weather systems and sediment movement on the beachface of a sandy beach.Mar. Geol. 79: 23–39.

Clarke, D. J., Eliot, I. G. and Frew, J. R., 1985. Variation in subaerial beach sediment volume on a small sandy beach over a monthly lunar tidal cycle.Mar. Geol. 58: 319–344.

Evans, G., 1965. Intertidal flat sediments and their environments of deposition in the Wash. Quart.J. Soc. London 121(482): 209–241.

Kutzbatch, J. E., 1967. Empirical eigenvectors of sea-level pressure, surface temperature and precipitation complexes over North America.J. Appl. Meteorol. 6: 791–802.

Katoh, K. and Yoshimatsu, A. 1984. A new method of three-dimensional empirical analysis for contour maps.Report of the Port and Harbour Research Institute 23(2): 28–47. (in Japanese)

MaCave, I. N., 1970. Deposition of fine-grained suspended sediments from tidal currents.J. Geophys. Res. 75 (21): 4151–4159.

Postma, H., 1961. Transport and accumulation of suspended matter in the Dutch Wadden Sea.Neth. J. Sea Res. 1(1/2): 148–190.

Reineck, H. E., 1967. Layered sediments of tidal flats, beaches, and shelf bottoms of the North Sea.In: Holocene Tidal Sedimentation G. de V. Klein (ed.), Dowden, Hutchinson & Ross Inc. Pennsylvania, USA, pp. 64–79.

Shenci, S. S. S., Murty, C. S. and Veerarra, M., 1987. Monsoon-induced seasonal variability of sheltered versus exposed beaches along the west coast of India.Mar. Geol. 76: 117–130.

Van Straaten, L. M. J. U. and Kuenen, Ph. H., 1957. Accumulation of fine grained sediments in the Dutch Wadden Sea.Geol. Mijnb. 19: 329–354.

Wang B. C. and Eisma, D., 1988. Mudflat deposition along the Wenzhou coastal plain in southern Zhejiang, China.In: Tide-influenced Sedimentary Environments and Facies, P. L. de Boer et al. (ed.), D. Reidel Publishing Company, Holland, pp. 265–274.

Wang B. C. and Eisma, D., 1990. Supply and deposition of sediment along the north bank of Hangzhou Bay, China.Neth. J. Sea. Res. 25(3): 377–390.

Winant, C. D., Inman, D. L. and Nordstorm, C. E., 1975. Description of seasonal beach changes using empirical eigenfunctions.J. Geophys. Res. 80: 1979–1986.

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

Standing crop and size structure of phytoplankton are strongly regulated by the turbidity maximum in the macrotidal Qiantang River estuary-Hangzhou Bay

Chlorophenols in marine organisms from the southern coast of Hangzhou Bay, China, and an assessment of risks posed to human health

Equilibrium coastal profiles: II. Evidence from EOF analysis

Significance test for empirical orthogonal function (EOF) analysis of meteorological and oceanic data

基于半经验模型的霍尔推力器壁面腐蚀形貌预测方法研究