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海洋各种气象分析

来源:钓鱼123  作者:渔乐在线  发表时间:2015-04-03 14:33:14112

一、黑潮洋流

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YANGLIUSHIHAISHUILIUDONGDEYIZHONGXINGTAI,QIFANWEIGUANGDA、XINGZHIWENDING,HUIDUIXINGJINGDEQUYUZHIHUANJING、QIHOU、SHENGTAISHENZHIWENHUACHANSHENGZHONGDAYINGXIANG。

南方双彩网彩票导航WEISHENMEHAISHUIHUICHANSHENGLIUDONG?YUANYINYOURUOGANZHONG:

(1)风吹影响。地球表面有大致上固定的行星风系(以全球为影响范围的地表风系)及比较不固定的、局部的打气扰动(如台风)。当一定方向和强度的风在海面吹过一段时间之后,因为摩擦力的作用,会使海水表面产生顺着风吹方向流动,而这表面水分子的流动,有会带动下层水分子跟着运动(但速度会渐减),因而产生水流。这叫做“吹送流”。

(2)海水密度差异。海洋各部的盐度和温度并非相等、恒定的,这些差异会造成水团的密度不同,而密度高的海水较重、密度低的海水较轻,所以会使海水产生流动。此种现象特成为“密度潮”。

(3)潮汐升降。受太阳和月球引力的影响,海水会出现周期性上升与下降的现象,这种水位升降引起的水流,称为潮流。

(4)补偿作用。海水是一种流体,而流体有连续性,因此当某处的海水流向他处时,周围的海水就要流过来弥补其缺,这就造成了补偿流。

NEIMEHEICHAOYANGLIUYOUSHIZENMEHUISHINI?

HEICHAOSHIYIGUSHILIPANGDADESHUILIU,TASHIBEITAIPINGYANGYANGLIUXITONGDEYIBUFEN,CHENGYINWEICHIDAOFUJINBIAOMIANHAISHUISHOUDONGBEIXINFENG(XINGXINGFENGXIDEYIYUAN)CHANGNIANCHUIFU,TONGSHIJIASHANGDIQIUZIZHUANDELIXINLI(KESHILI)YINGXIANG,ZAICHIDAOBEICEXINGCHENGYOUDONGWANGXILIUDONGDE“BEICHIDAOYANGLIU”。CIYANGLIULAIDAOYAZHOUDALUDONGANSHISHOUDAOZUDANG,YIBUFENHUIZHUANXINGCHENGCHIDAONILIU,YIBUFENZHUANXIANGBEIFANGYANZHETAIWANDAO、RIBENDAOQUNYUNDONG,ZHEIBUFENJIUSHIDAJIASHUZHIDEHEICHAO。

HEICHAODAODARIBENBEIFANGHOU,SHOUXIFENG(YESHIXINGXINGFENGXIDEYIYUAN)CHUIFUERZHEXIANGDONG,CISHIBEICHENGWEIBEITAIPINGYANGYANGLIU。BEITAIPINGYANGYANGLIULAIDAOBEIMEIDALUXIANSHI,YIGUZHUANXIANGBEIFANG,CHENGWEIALASIJIANUANLIU,LINGYIGUYANMEIGUOXIANLIUXIANGNANFANG,CHENGWEIJIALIFUNIYALIANGLIU,ZHEIGUSHUILIUZUIHOUHUIHUIGUIDAOBEICHIDAOYANGLIUZHONG。

HEICHAOLAIZICHIDAO,XIANGDUILAISHUOTADEWENDUXIANGDANGGAO(XIAJIBIAOCENGSHUIWENKEDA30℃,DONGJIYEBUDIYU20℃。)YINCIBEICHENGWEI“NUANLIU”。TANENGWEILIUJINGDEDIQUDAILAIWENNUAN、CHAOSHIDEQIHOU,TONGSHIYEXIEDAIZHEDALIANGHUIYOUXINGYULEI(LIRUMEINIANCHUNXIAZHIJIANCHUXIANYUTAIWANDONGCEHAIYUDEHEIWEIYU)。ZAILIUDONGGUOCHENGZHONG,SHOUDIXINGYINGXIANGHUOYINBUCHANGZUOYONGERCHANSHENGDE“YONGSHENGLIU”,HAIHUIJIANGHAIDIDEYINGYANGYANDAIDAOSHANGCENGSHUIYU,XIYINGELEISHENGWUDALIANGJUJI,YINCIKESHIYUHUOFENGFU。

二、潮汐的成因与影响

LAOJINGYANDIAOZHECHANGSHUOCHUMENXIAGANYAOKAN“LIUSHUI”,ZHEIGELIUSHUI,ZHIDEJIUSHICHAOXI。

南方双彩网彩票导航DAJIADOUZHIDAO,CHAOXIXIANXIANGSHIYUELIANGYUTAIYANGDEYINLIZAOCHENGDE,DANWEISHENMEHUIYOUDACHAO、XIAOCHAOZHIFEN?WEISHENMEMEITIANHUIYOULIANGCIZHANGTUI?ZHANGCHAOYOUSHISHENME?

(1)所谓“潮汐”。古人把发生在白天的海水涨落现象称为“潮”,发生在晚上的称为给“汐”,两者合称潮汐。

(2)潮汐的涨退。南方双彩网彩票导航海水从较低的水位开始上升到较高的水位,这段过程叫涨潮,从较高水位开始下降之低的水位,这段过程则是退潮。当水位上涨到最高点时,称为满炒或高潮,当下降到最低点时,称为干潮或低潮。另外在水位到达满朝或干潮点时,通常会有一段时间海面无升降现象,这叫做停潮或平潮。

(3)潮位的高低。不同地方在同一潮水中,水位的高低并不全一样,而同一地方在不同日子里面,潮水的高低也会变动。

BUTONGRIZIDESHUIWEICHAYI,ZHUYAOSHIYOUYUEQIU、TAIYANGJIDIQIUDEXIANGDUIWEIZHIBUTONGZAOCHENG。ZAINONGLISHUORIHUOWANGRI(XINYUEHUOMANYUE),YUEQIU、TAIYANG、DIQIUSANZHEYUELVEPAICHENGYIZHIXIAN,CISHIYUEQIUHETAIYANGTONGZAIDIQIUYICEHUOXIANGDUIDELIANGCE,YOUYUWANYOUYINLIDEZUOYONG,FASHENGMANCHAOYUGANCHAOSHUIWENCHAJUZUIDADEXIANXIANG,CISHICHENGWEI“DACHAO”。(DANSHIJISHANGHUIYANHOULIANGSANTIAN)。DAOKANSHANGXIANYUEHUOXIAXIANYUE(NONGLICHUQI、BA、YIJINIANER、NIANSANRI)SHI,YUEQIU、TAIYANG、DIQIUSANZHEYUELVEPAICHENGZHIJIAOSANJIAOXING,CISHIMANCHAOYUGANCHAOSHUIWEICHAJUZEZUIXIAO,JISHI“XIAOCHAO”。

ZHIYUMANCHAOYUGANCHAOSHUIWEIDECHAJUJIAOZUOCHAOCHA,TONGYIDIDIANDEMANCHAYEYOUZHOUQIXINGBIANHUA,HUIYOUXIAOBIANDA,ZAIYOUDABIANXIAO,ZHEIZUIGAOCHAOWEIYUZUIDICHAOWEIZHIJIANDEJULI,JIAOZUOCHAOJIANDAI。

(4)潮汐的周期。潮汐每天干满的时间都不一样;同一地前后两次满朝或两次干潮之间的间隔,约为12时25分,换句话说,潮水从干潮开始上涨到满朝,约需6小时多(反之亦然),而前后两天潮水的事假,则会延迟约50分钟,这叫做潮迟率。

(5)潮汐的形态。每天有两次满朝、两次干潮者,称为半日潮;每天仅有一次高潮一次低潮的,称为全日潮。如果一个地区的实际潮汐现象并不单纯为半日潮或全日潮的,就叫做混合潮。

南方双彩网彩票导航ZAIQUANRICHAOXIANXIANGJIAOMINGXIANDESHIHOU,YITIANZHIZHONGCONGMANCHAODAOGANCHAOHUOCONGGANCHAODAOMANCHAODESHIJIANJIANGBI6XIAOSHIYAOZHANGDEDUO,CIJISUCHENGDE“ZHANGCHAO”。

(6)那么潮汐现象对钓鱼活动有何影响呢?

①CHAOXIZHANGTUISUISHIHAIMIANDECHUIZHISHENGJIANG,DANZAIDIXING、HAIFENG、DIQIUZIZHUAN、ZHONGLIZUOYONGDENGYINSUXIANGHUYINGXIANGXIA,QUEHUIZAOCHENGHAISHUIDESHUIPINGYIDONG,HUANYANZHIJIUSHIZAOCHENGLEHAILIU,ERHAILIUSHISHIWUBANYUNDEZHONGYAOTUJING,DANGTINGCHAOJIEDUANSHUIXIALIUSHI,SHIWUJIUBUHUIBEIYUNSONGDAOGEDI。YULEIZHANGQISHENGHUOYUHAIYANGZHONG,ZAOXIGUANGENJUSHUILIULAIDIAOZHENGZUOXI,SUOYITAMENZAIZHEIDUANSHIJIANWANGWANGHUIZIDONGTINGZHIJINSHI。

南方双彩网彩票导航②DANGCHAOXIZHUANHUANSHI,HAILIUFANGXIANGWANGWANGYEGENZHEGAIBIAN,ZHEIYIWEIZHESHIWUBEIYUNSHUDEQUCHUYEBIANLE,SUOYIYUQUNDANGRANHUIGENZHEYIDONG。

③JIDIAOCHANGSUOHAIDIDIXINGBIANHUAJIDA,JIRANHAILIUFANGXIANGYIGAI,BIAODIANZISHIWANQUANBUTONG,YINCIDIAOZHERUGUODUICHAOSHUIMEIYOUCHONGFENDERENZHIYUZHANGWO,CHENGJIBIRANBUHUILIXIANG。

三、近岸水流

CHULEHEICHAOYANGLIUJICHAOXIXIANXIANGWAI,JINANSHUIYUDEHAISHUILIUDONGZHUANGTAIYEDUIDIAOYUYOUZHONGDAYIYI。

LIUDONGDEHAISHUIYULUYUHUANJINGJIHAIDIJIECHUHOU,HUIFASHENGXUDUODUIDIAOYUYOUZHONGDAYINGXIANGDEBIANHUA,ZHEIXIEBIANHUAYIDIAOYUQUANXIGUANDECHENGHULAISHUOKEYOUYIXIAJIZHONGMINGCHENG:

(1)本流。所谓“本流”,并不是某种性质流水的特定称呼,而是相对来说在一个区域内比较强大的、速度快的、最主要的一股水流。通常那种方向固定(意指在涨潮阶段或退潮过程中方向固定,但潮水转换后方向即可能改变。)且流速明显高于周边其他水流的,就会被称为本流。

南方双彩网彩票导航ZAIZHEIZHONGLIUSHUIZHONG,FUBIAODIAOZHEBIJIAONANWEICHIGUDINGWEIZHIHUODIAOPENGSHENDU,YOUXIESHUISHITEBIETUANJIDESHUIYU,JISHIYONGKONGLONGDANHUOGAOZAIZHONGDEZHANGBIAOYEYIYANGHUIBEIXUNSUDAIZOU,DIAOYOUCHANGCHENGZHEILEILIUKUANGWEI“LIUGOU”。BUGUOBINGBUSHISUOYOUDEDIAOCHANGDOUYOUBENLIUCUNZAI,YOUXIEDIFANGHAISHUIDEDONGTAIBIJIAOHUANMANHUOWENLUAN,DIAOYOUJIUBUHUIBAQIZHONGYIGUSHUILIUJIEDINGWEIBENLIU。

(2)支流。这“支流”二字也不是专有名词,而是相对于本流而言比较小区域的、流速慢的、方向较多变化的水流。此类水流有沿着海岸推送的,也有冲向海岸或往外流出的,支流不一定都是本流的分支,它的形成还受风力、波浪、潮汐现象等因素的影响,且会因海岸地形、海底状态的影响而改变它的方向、速度、规模。

(3)回流带。南方双彩网彩票导航运动中的水流如果碰到地形改变(例如内湾、凸岬),或海域深度出现变化(如有暗礁或深沟),都容易在这个水域内形成一个翻涌打转的水团,这就是“回流带”。回流带的规模会随水流而变,水流越急,回流带范围就越广、形态越明显,水流越缓,则回流带有可能微弱到看不出来。回流带特容易让海中漂行的食物留下来打转。

(4)反拨潮。一道道涌向岸际的波浪,带着大股大股的海水打上礁石,然后再翻身灌回大海,这些水必须有个路径流出去,沿此路径流出去的海水就叫做“反拨潮”。其方向均为从岸边往外海流出,能够将岸上的有机物冲刷入海并带出去,故具有吸引沿岸鱼只的强大魅力。寻找反拨潮的方法很简单,只要注意观察破浪造成的白泡沫,假如白泡沫会形成一条持续往外拖出相当距离的白泡沫,那就是了!

(5)潮目。所谓“潮目”,就是方向或流速不同的两股(或两股以上)流水相互交错、撞击、摩擦,因而造成一个表面比较平整无波、看似甚少流动、杂物容易停滞的水区。这种水区就如同海洋中的十字路口,是鱼群和食物交会、聚集之处,所以常为下竿的标点。

1、地形

YANANHAIYUDEDIXINGBIANHUAHUIDUIDIAOYUHUODONGGOUCHENGYINGXIANGDEZHUYAOYOULIANGDIAN,QIYISHIHAIANXIANDEQUZHIAOTU,LINGYIGEJIUSHISHUIYUSHENDUDEBIANHUA。

(1)海岸线。单调平直的海岸线,常按时水下环境缺少变化(沙滩就是典型的例子),同时这类水区水流方向多半平行于海岸,流速稳定,没有食物在此聚集打转,因此鱼群也不会集中在这里。而曲折凹凸明显的环境,因为水流、波浪等的变化十分丰富,很容易形成回流带、反拨潮、潮目等吸引鱼群的条件,故垂钓丰收的可能性显然比单调平直处高。

(2)深度变化。南方双彩网彩票导航海域深度不仅关系到鱼类对水压的适应能力,同时对海水的温度、水色、盐度、透明度以及水流方向、速度等等也都有明显影响,所以也会影响鱼类的栖息与活动方式。

南方双彩网彩票导航JULILAISHUO,BIAOMIANPINGZHENG、QUEFAAOTUQIFUDEYANSHICENG、BULUNQIPODUSHIPINGHUANHUOSHIDOUQIAO,SHENZHIRUDUANCENGNEIYANGCHUZHIXIANGSHUIXIAYANSHEN,ZHEIYANGDEDIXINGYONGCHANGDOUBURONGYIXIYINYULEIZHULIU。DANZHEIPINGTANDIYURUOCHUXIANAOXIAN、GUGOUHUOLONGQI,NEIMEAOGOUZHIZHONGHELONGQIBUWEIDEJIBU,JIUHUICHENGWEIDICENGHUODONGYULEIXIHUANQIXIDECHANGSUO,ERLONGQIDEDIXINGYOURONGYIZAOCHENGHAILIUYONGSHENG,SHISHENCHUDESHIWUBEIDAIDAOQIANCHULAI,SUOYIQISHANGFANGYECHANGCHENGWEIBIAOCENGHUODONGYULEIJUJIDECHANGSUO。

2、底质

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(1)栖息方式。南方双彩网彩票导航有些鱼类终其一生不会跟海底发生接触,因为他们的食物也是在海洋的上层活动,这些鱼类通常被称为外洋或表层洄游性鱼。但矶钓的目标物多半不属于这些鱼群,而是接近海底或甚至直接生活在海底的种类。这些鱼种有的干脆趴在海底,如鲆鲽类(比目鱼)、魟鳐类(魔鬼鱼);有的则喜欢躲在缝隙中,如石斑、海鳗等;有的习惯白天四处乱闯,晚上就找个洞穴睡觉,如鹦哥鱼类就多半属于这种。但更多的鱼种是以这类充满变化的底质环境作为栖息基地,安全时跑出来享用附近丰盛的食物,遇到危险就迅速进入屏障躲避。

BUGUOSHANGSHUYULEIZHONG,MEIYIZHONGYUDUIHUANJING(DIZHI)DEXUANZEHAISHIHUIYOUCHAYI,LIRUHEIDIAOXIHUANSHENGHUOZAIJIAOSHAHUNHEDIDAI、JIANAPIANHAOSHILIDIXING,HEIMAOZEQINGXIANGJUJIZAICHUNCUIYANJIAODEQUYU。

(2)生殖行为。大多数鱼类是卵生的,但也有胎生或介于卵生与胎生之间的卵胎生者。不论他们是哪一种生殖方式,选择一个适合繁殖的环境,广义来说需要考虑交配前的营养补给、卵或仔鱼生长所需环境,繁殖后亲鱼的体力恢复等项。

南方双彩网彩票导航YULEIDELUANYOUPIAOFUXING、CHENJIANGXINGHENIANZHEXINGDENGQUBIE。PIAOFUXINGLUANXUYAOSHIDANGDESHUILIULAIDAIYINYULUAN,PIAODAOHESHIYOUYUCHENGZHANGJIN、JINSHIZHICHU。CHENJIANGXINGLUANXUYAOHAIDIYOUZUGOUDEXIAOJIANXI(RULISHIDIXING)RANGTAMENLUOJIAO,QIELUOJIAOBIXUANDINGWENGUYOUYOUTONGCHANGDESHUILIU,FOUZELUANLIHUIBEICHONGZOUHUOFUBAI,NIANZHEXINGLUANZEGENGXUYAOANDONGWENGUQIESHUILIUSHUNCHANGDEHUANJING,TONGSHIHAIBIXUYOUZUGOUDEYINBIXING,BURANYULUANHENKUAIJIUHUIBEIQITAYUCHIGUANG!

ZHIYUJIAOPEIQIANHOUDEJINBU,BUYONGSHUOSHIGENSHIWUFENGQIANZHIJIEXIANGGUANDE,ERJIDIAOMUBIAOYUZHONGDESHIWULAIYUAN,YOUHENDAYIBUFENSHIZHIJIEFUZHEYUDIZHISHANGDE,RUZAOLEI、JIAQIAOLEI、BEILEIDENGDENG,SUOYIDIZHIDEYINGXIANGFEICHANGZHONGDA。

关于风的尝试

DONGYA—TAIPINGYANGDIQUSHITIANQIDUOBIANDEQUYU,YITAIWANFUJINLAIKAN,MEINIANDAZHIHUICHENGYIXIADEZHOUQIXINGBIANHUA:YUESANYUEZHIHOU,TAIYANGZHISHEWEIZHICONGCHIDAOWANGBEIYANSHEN,CUSHIBEIFANGDALUSHANGDEXIBOLIYALENGGAOYAQIANGDUJIANRUO,TAIPINGYANGGAOYAZERIJIANFADA,YINCIDONGBEIJIFENGSHILIRIJIANXIAOTUI,XINANFENGKAISHIQUDAIZHI;WULIUYUEJIAN,HAIYANGYUDALUQITUANXIANGHUTUIJI,ZAITAIWANFUJINXINGCHENGZHILIUFENG,ZAOCHENGSUOWEIDEMEIYUJI;QIBAYUEJIANTAIPINGYANGGAOYADESHILIDADAODINGFENG,TAIWANDIQUYIXINANJIPIANNANFENGWEIZHU,DANCIQIJIANHAIYANGSHANGRONGYIYINDALIANGSHUIQIZHENGFAERCHUXIANREDAIXINGDIQIYA,DANGZHEIDIQIYAQIANGDUDAODAYIDINGCHENGDUSHI,JIUXINGCHENGLETAIFENG,SUOYIZAIQI、BA、JIU、SHIYUEZHIHOU,TAIYANGZHISHEWEIZHIWANGNANYIDONG,KUAYUECHIDAOJINRUNANBANQIU,SHIDETAIPINGYANGGAOYAZHUJIANJIANRUODONGTUI,BEIFANGDALULENGGAOYAZHONGXINQUDEYOUSHI,DAOZHIDONGBEIJIFENGKAISHINANXIA,BINGYUSHIERYUEZHIYINIANERYUEJIANZHUZAICIDIQUDETIANQI。

YOUSHANGSHUGUILVKEZHI,YINGXIANGDONGYA—TAIPINGYANGDIQUDEFENGHUOTIANQIXITONG,ZHUYAOYOUYIXIAJIZHONG:

(1)东北季风。基本上来自西伯利亚的大陆,低温且干燥,所含水汽及冰晶的形态存在于高空中,但当它东移出海时,却会被加温,且沿路吸收水汽,因而天气会变成阴霾、风大、有小雨,并且在其前缘造成一条风力强劲的冷锋面。

(2)梅雨锋面。由太平洋暖气团鱼大陆冷气团相互推挤形成的梅雨锋面,由于扰动剧烈且带有大量的水汽,故常引起明显风变及降雨。当太平洋高压势力较强时,滞留锋会被往西北推移,台湾地区受到海洋性气团笼罩,天气就会比较晴朗炎热。若是大陆冷高压势力交强,则滞留锋会往东南移动,台湾地区天气就变得阴雨不断。

(3)台风。台风的危害不用多说了,但它有三种经常被忽视的副作用不得不提,那就是西南气流、长浪和暴潮。

XINANQILIUGENXINANJIFENGBUTONG,JIFENGSHIZHIJIAOZHANGSHIJIAN、JIAODAFANWEICHIXUCHUIFUDEFENG,QILIUZESHIDUANZAIQIEBIANHUADADEQIHOUXIANXIANG。TAIFENGJINGGUOTAIWANDIQUHOUHOU,YINQINISHIZHENZHUANDONGDETEXING,HUIYINRUWANGSHENGDEXINANQILIU,ERZHEILAIZINANHAIDEQILIUDAIYOUDALIANGSHUIQI,YINCICHANGZAOCHENGYANZHONGZAIHAI。

ZHANGLANGSHIYIZHONGBOZHANGFEICHANGCHANGDELANG,CHANGYOUTAIFENGDEQIANGDAFENGLIYIJIDIYASUOYINQI,KECHUANBODAOXIANGDANGYAOYUANZHICHU,QIEQUTUIJINSUDUBITAIFENGBENSHENYIDONGDESUDUKUAIHENDUO,YINCIDUIDIAOKEDEANQUANYOUZHEJIDADEWEIXIE。

南方双彩网彩票导航BAOCHAOWEITAIFENGYINQIDELINGYIGEDAMAFAN,QICHENGYINGENQIANDUANSUOYANLEISI,YOUYUTAIFENGZHONGXINQIYASHENDI,HAISHUIHUIBEIXIQISHIHAIMIANSHENGGAO,ZAIJIASHANGQIANGJINGFENGSHICHUIGUA,HAISHUIYINDUIJIZUOYONGGENGJIAGAOZHANG,CISHIRUOZAIFENGZHANGCHAO,JIUHUIDUIYANHAIDIQUZAOCHENGHAISHUIDAOGUANDEZAIHAI。

海洋各种气象分析

(4)西南季风。在亚洲大陆东岸、太平洋西侧水域,夏季若无台风或热带性低气压时,通常呈现晴朗炎热、西南风微弱的天气。这种季风的影响乍看不是很明显,但因为太阳持续对地表加入又缺乏风来调节,地表附近产生旺盛的上升气流,往往很快就发展成一个高大数千甚至上万米、顶部呈砧状的巨大云柱,此种内部饱含大量水汽的积雨云,在高空被冷却后,会形成急速且雨量大的雷雨,而且这种降雨因为带着冷空气向下冲,故能引起强烈的风变,形成到达八九级以上的阵风。

关于浪的常识

南方双彩网彩票导航HAILANGSHIHAISHUISHOUWAILIZUOYONGHOUXINGCHENGDEZHENDANGXIANXIANG。QIZUIMINGXIAN、ZUIPUBIANDECHENGYINJIUSHIFENG。DANHAIYOUHENDUOZHONGWAILIYEHUIYINQIHAILANG,LIRUDIQIAOBIANDONG、HAIDIHUOSHANBAOFA、CHAOXIDENG。

南方双彩网彩票导航BOLANGSUIRANHUIYOUFASHENGDEDIDIANXIANGWAIKUOSAN,DANSHUIFENZIBINGMEIYOUSUIZHEBODECHUANDIERYIZOU,TAMENZHIZAIYUANCHUZUOSHANGXIAYUNDONG。BOLANGDELINGYIGETEBIEXIANXIANGSHIQIYINGXIANGDESHENDUDAYUEXIANGDANGYUTADEBOZHANGDEYIBAN,YIJIRUGUOMOUCHUFASHENGLEBOFENGYUBOFENGJIANJULIWEI10MIDEHAILANG,NEIMEZAISHUISHENCHAOGUO5MIDESHENCHU,JIUGANJUEBUDAOTADEDONGTAILE。

YISHANGSHIBOLANGYIBANXINGZHIDEJIANLVEMIAOSHU,DIAOYOUHAIJIDEQIANJIETIDAODE“ZHANGLANG”BA?SUOWEIZHANGLANG,SHIYIZHONGLAIZIYUANFANGHAIYU、YIJINGTUOLIQIFAYUANDI(LIRUYOUYUANCHUTAIFENGSUOYINQI)DEHAILANG。ZHEIZHONGLANGDEBOZHANGFEICHANGZHANG,XINGTAIKANQILAIYUANHUAHEHUAN、LANGTOUBUGAO,YINCIRENMENCHANGHULVETADEWEIXIANXINGHUOBURONGYICHAJUEQIDAOLAI,DANTASUOYUNHANDENENGLIANGJIWEIKEGUAN,ZAIXINGJINTUZHONGSHUAIJIANDEBUDUO,SUOYINENGGOUYINGXIANGDAOHENYUANDEDIFANG。

南方双彩网彩票导航DANGZHEIZHONGZHANGLANGTUIJINDAOLUDIFUJINSHI,YINWEIHAIYUSHENDUBIANQIAN,BOLANGZHONGYUNXUDEDONGNENGJIUKAISHIZHUANBIANWEISHINENG,SHIBOZHANGSUODUAN、BOFUJIADA,YEJIUSHISHUOHAISHUICHUXIAN“XIANGSHANGDUIDIE”DEXIANXIANG;SHUISHENBIANDEYUEQIAN,DUIDIEGAODUJIUYUEGAO,TONGSHIYOUYINWEIHAIDIMOCADECHIZHI,SHISHENCHUDEBOCHUANDISUDUMANYUBIAOMIAN,YUSHILANGXINGYEBIANDEQIANQING,ZHONGZHILANGFENGWUFAZAIWEICHIWENDINGZHUANGTAIERBENGKUI,DALIANGHAISHUIMENGRANZASHANGANBI。

南方双彩网彩票导航 ZHEIXIANXIANGRUGUOFASHENGZAIDOUQIAO、JISHENDEYANSHIHAIANHUOFANGBODIQIANDUAN,YOUYUSHENDUSHIZAIDUANJULINEIXUNSUBIANQIAN,BOFENGZHAYANJIANJIUYOUKENENGDIEGAODAOCHAOGUORENMENLIZUDIANDECHENGDU,HAILANGJIAZHEDALIANGSHANGWEISHIFANGDEDONGNENGYUSHINENG,YIGUNAOZHUANGSHANGZOUBIBUJIDEDIAOKE,YUSHIDIAOKELUOHAISHIJIANJIUFASHENGLE!

风速与浪高对应关系表

风速与浪高对应关系表

ZAISHENDUBIANHUAHUANHEDESHADUIDIDAIYIBANDEZHANGLANGYINGXIANGDUOBUHUIHENYANZHONG,DANRUOLAIXIDELANGSHIYOUQIANGLIEHAIDIDIZHENSUOYINFA,NEIMETAJIUYOUKENENGZAOCHENGRU2004NIAN12YUE26RINANYADAHAIXIAOBANDESHANGHAI!

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