WATER MASSES OF KUALA TERENGGANU COASTAL WATERS

Publish Year: 1383
نوع سند: مقاله کنفرانسی
زبان: English
View: 1,624

This Paper With 6 Page And PDF Format Ready To Download

  • Certificate
  • من نویسنده این مقاله هستم

استخراج به نرم افزارهای پژوهشی:

لینک ثابت به این Paper:

شناسه ملی سند علمی:

ICOPMAS06_074

تاریخ نمایه سازی: 5 آذر 1384

Abstract:

In order to identify the water mass, a plot of temperature versus salinity data, from near the surface to the bottom or T-S diagrams can used[1],[4],[5]. This powerful analytical technique was introduced into physical oceanography by B. Helland-Hansen in 1916. In the 1930s the T-S method was extensively used to identify various water masses in the world ocean [9]. Excellent generalization was made by Svrdrup . Johnson and Fleming(1942) to describe layering of water masses that common vertical salinity and temperature distribution , as denoted by their T-S curves [9] also can say each water mass can be identified on the basis of temperature and salinity values at various subsurface depths(pressure).each water mass can be identified by a line that converges to a common point[2]. Saadon and Alejandro (1996) reported that during the northeast monsoon seasons there are two different water masses with lower temperature and salinity than during the south west monsoon.Marghany and Pishgahi (2004) made a study about water masses properties along coastal water of kuala Terengganu . they reported, in general there are two water masses below surface to mid of depth. Pishgahi and Marghany (2004) studied about water masses in south china sea off Pahang .They reported that there are four water masses in that study area ,two water masses inshore and two water masses offshore during pre monsoon. The onshore water masses have a low salinity than offshore because the water discharge from mouth river of Pahang river generate onshore water masses. The aim of this investigation is to study the seasonal water mass variations , pre monsoon and post monsoon ,in South China Sea , by using 2 series data such as temperature , salinity and density or sigma_t (σt) observed by sampling.

Authors

ASGHAR PISHGAHI

MSc.,Physical Oceanography,KUSTEM, Malaysia; BEng., Mechanical Eng.,Azad Univ.,Iran

MAGED MARGHANY

PhD in Environmental Remote Sensing ; MSc. in Physical Oceanography, UPM, Malaysia

مراجع و منابع این Paper:

لیست زیر مراجع و منابع استفاده شده در این Paper را نمایش می دهد. این مراجع به صورت کاملا ماشینی و بر اساس هوش مصنوعی استخراج شده اند و لذا ممکن است دارای اشکالاتی باشند که به مرور زمان دقت استخراج این محتوا افزایش می یابد. مراجعی که مقالات مربوط به آنها در سیویلیکا نمایه شده و پیدا شده اند، به خود Paper لینک شده اند :
  • Apel, J.R., Principles of Ocean physics, 3" ed., Academic Press ...
  • _ J.M., Applied Oceanography, 1*" ed., John Wiley &sons, Inc.: ...
  • iur, H.B., Jacobs, G.A. and Teague, W.J. *Montly variations of ...
  • Knuss , John A. Introduction to Physical _ ed., prentice-hall ...
  • Maged, M.M. and Pishgahi, A., ^Water masses properties along Malaysian ...
  • _ _ course team. Ocean circulation, 1* ed. The Open ...
  • Pishgahi, A. and Marghany, M.M. _ Water masses properties along ...
  • Saadon, N.M, and C., Alej andro , 'Interannual and Seasonal ...
  • _ Elements of Dynamic _ ed. Allen & Unwin :Boston, ...
  • نمایش کامل مراجع