海洋通报
海洋通報
해양통보
MARINE SCIENCE BULLETIN
2014年
2期
126-131
,共6页
磨刀门河口%亚潮%小波分析%小波相干
磨刀門河口%亞潮%小波分析%小波相榦
마도문하구%아조%소파분석%소파상간
Modaomen Estuary%sub-tide fluctuations%wavelet analysis%wavelet coherence
根据珠江河口磨刀门水道的三灶站、大横琴站、灯笼山站、竹银站2010年全年的逐时潮位资料,利用小波分析方法研究磨刀门河口区亚潮变化的周期特征。采用小波相干方法,分析亚潮与气压、风速、流量之间的相关关系。研究结果表明:(1)磨刀门河口亚潮主要存在5~6 d、14 d、21 d周期性波动。(2)亚潮5~6 d的周期波动的能量来源于气象要素及入海径流;亚潮14 d左右的周期波动的能量来源于天文大小潮、气象要素及入海径流的叠加效应;磨刀门水道下游站点亚潮21 d的周期性波动受到气象要素及入海径流的联合作用,而上游站点亚潮21 d的周期性波动主要受到入海径流因素的影响。(3)在不同季节,亚潮对气象要素的响应情况会产生不同影响。
根據珠江河口磨刀門水道的三竈站、大橫琴站、燈籠山站、竹銀站2010年全年的逐時潮位資料,利用小波分析方法研究磨刀門河口區亞潮變化的週期特徵。採用小波相榦方法,分析亞潮與氣壓、風速、流量之間的相關關繫。研究結果錶明:(1)磨刀門河口亞潮主要存在5~6 d、14 d、21 d週期性波動。(2)亞潮5~6 d的週期波動的能量來源于氣象要素及入海徑流;亞潮14 d左右的週期波動的能量來源于天文大小潮、氣象要素及入海徑流的疊加效應;磨刀門水道下遊站點亞潮21 d的週期性波動受到氣象要素及入海徑流的聯閤作用,而上遊站點亞潮21 d的週期性波動主要受到入海徑流因素的影響。(3)在不同季節,亞潮對氣象要素的響應情況會產生不同影響。
근거주강하구마도문수도적삼조참、대횡금참、등롱산참、죽은참2010년전년적축시조위자료,이용소파분석방법연구마도문하구구아조변화적주기특정。채용소파상간방법,분석아조여기압、풍속、류량지간적상관관계。연구결과표명:(1)마도문하구아조주요존재5~6 d、14 d、21 d주기성파동。(2)아조5~6 d적주기파동적능량래원우기상요소급입해경류;아조14 d좌우적주기파동적능량래원우천문대소조、기상요소급입해경류적첩가효응;마도문수도하유참점아조21 d적주기성파동수도기상요소급입해경류적연합작용,이상유참점아조21 d적주기성파동주요수도입해경류인소적영향。(3)재불동계절,아조대기상요소적향응정황회산생불동영향。
According to the data of hourly tidal level from the Sanzao Station, Dahengqin Station, Denglongshan Station and Zhuyin Station located in the Modaomen watercourse of the Pearl River in 2010, the wavelet analysis method was used to study the periodical characteristics of the sub-tide oscillation in the Modaomen Estuary. By use of the wavelet coherence method, the relationship between sub-tide and barometric pressure, wind speed and river discharge was analyzed. The results showed that: (1) The sub-tide fluctuation periods with 5-6 d, 14 d and 21 d existed in the Modaomen Estuary. (2) The energy of the periodical fluctuations of 5-6 d for sub-tide came from meteorological elements and river discharge;and the energy of the periodical fluctuations of 14 d came from the superimposed effect of the astronomical spring-neap tide, meteorological elements and the river discharge;the periodical fluctuations of 21 d were affected mainly by the joint action of meteorological elements and discharge. However, the fluctuations of 21 d in the upstream station were mainly affected by the river discharge. (3) Sub-tide in different seasons would show different responses to meteorological elements.