Ocean-Atmosphere Observations in Philippine Sea by Moored Buoy

A. Nagano, I. Ueki, T. Hasegawa, K. Ando
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引用次数: 2

Abstract

Offequatorial extension of equatorial buoy arrays such as Tropical Atmosphere and Ocean/Triangle Trans-Ocean Buoy Network (TAO/TRITON) buoy array is required to monitor global and regional climates. On December 3, 2016, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) deployed a moored buoy (Ph buoy) at 13°N, 137° E in the Philippine Sea and are measuring temperature, salinity, and dissolved oxygen concentration from the sea surface to 300 m and atmospheric parameters. The Philippine Sea is located in the northern edge of the western Pacific warm pool, where atmospheric and oceanic disturbances on timescales from days to decades such as typhoons, cold surges, seasonal march of the East Asian monsoon, Madden-Julian Oscillation, El Niño and Southern Oscillation, and Pacific Decadal Oscillation occur. Global and regional climate changes possibly increase the frequency of occurrences of extreme weather events. Sensors installed on the buoy tower observed tropical depressions in the winter of 2016/2017. In addition, the development and annihilation of the barrier layer, which exists between the bases of the isothermal and mixed layers, were observed by the underwater sensors. The data collected at this mooring site serve to researches on extreme weather events.
菲律宾海系泊浮标海洋大气观测
赤道浮标阵如热带大气和海洋/三角跨洋浮标网(TAO/TRITON)浮标阵需要向赤道外延伸,以监测全球和区域气候。2016年12月3日,日本海洋地球科学技术机构(JAMSTEC)在菲律宾海13°N, 137°E部署了一个系泊浮标(Ph浮标),测量从海面到300米的温度、盐度和溶解氧浓度以及大气参数。菲律宾海位于西太平洋暖池的北部边缘,在数天至数十年的时间尺度上,发生了台风、寒潮、东亚季风的季节性进行期、马登-朱利安涛动、厄尔尼诺Niño和南方涛动以及太平洋年代际涛动等大气和海洋扰动。全球和区域气候变化可能增加极端天气事件发生的频率。安装在浮标塔上的传感器在2016/2017年冬季观测到了热带低气压。此外,利用水下传感器观测了存在于等温层和混合层基底之间的势垒层的发展和湮灭过程。在这个系泊地点收集的数据用于研究极端天气事件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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