太平洋赤道 meaning in Chinese
equatoral pacific
Examples
- Abstract : the sea - surface temperature change in october along the eastern pacific equator is obviously counter - correlation to the western pacific ridge line of the subtropical high of the coming early summer ( june ) ; the sea - surface temperature annual change has a sensitively instructive meaning on the precipitation of the coming flood season in qingdao area
文摘:历年10月东太平洋赤道附近的海温变化与来年初夏( 6月)西太平洋副高脊线位置呈明显的反相关；其海温的年际变化对于青岛地区来年汛期降水具有敏感的指示意义。 - When the wpi - soi correlation is weak and the west pacific sst warmer ( colder ) , a anomalous anticyclonic ( cyclonic ) circulation is found in the lower troposphere over northern equatorial western pacific . this anomalous circulation is not in favor of maintaining a significant correlation between the west pacific sst and enso
Wpi - soi相关关系微弱时，在西太平洋赤道北侧的对流层低层存在高(低)海温?反气旋(气旋)异常环流系统，不利于维持enso与西太平洋海温变化间的紧密联系。 - Based on the epwp and wpwp in conjunction with abnormal north and west wind , a new possible iii mechanism is provided for the evolution of the 1997 / 1998 el nino . to be specific , the warm kelvin wave propagating to east excited by the abnormal west wind can suppress the cold upwelling flow in the eastern pacific , which , in turn , is favorable to the eastern pacific sst increase ; abnormal west wind can make the warm water of the wpwp east edge extend to east , which is conductive directly to eastern pacific sst increase ; the abnormal west wind propagating to east can make the sea surface warm water near two equatorial laterals converge to the equator by ekman drifting , which , in rum , strengthens the downwelling flow near the equator , leading to eastern pacific sst increase
将东、西太平洋暖池及异常北风、西风一并结合起来考虑，提出1997 1998elnino事件发生、发展的一种新的可能机制：异常西风激发东传的暖kelvin波对东太平洋的冷上翻流有抑制作用，从而有利于东太平洋海表温度增加；异常西风驱动西太平洋暖池东端暖水向东伸展直接有利于东太平洋海表温度增加；东传的异常西风可以通过埃克曼漂流效应将赤道两侧的海表暖水向赤道辐合从而加强了赤道附近的下沉流，也有利于东太平洋赤道附近海表温度增加。