1.0Institute of Oceanography, NTUhttps://www.oc.ntu.edu.tw/en/rich600338<blockquote class="wp-embedded-content" data-secret="lB7D36sRJr"><a href="https://www.oc.ntu.edu.tw/en/research-highlights/34862/">Seasonal Variation of CO2 air-sea flux and Effects of Warming in the Kuroshio Current of the East China Sea</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.oc.ntu.edu.tw/en/research-highlights/34862/embed/#?secret=lB7D36sRJr" width="600" height="338" title="“Seasonal Variation of CO2 air-sea flux and Effects of Warming in the Kuroshio Current of the East China Sea” — Institute of Oceanography, NTU" data-secret="lB7D36sRJr" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script> /*! This file is auto-generated */ !function(d,l){"use strict";l.querySelector&&d.addEventListener&&"undefined"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!/[^a-zA-Z0-9]/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret="'+t.secret+'"]'),o=l.querySelectorAll('blockquote[data-secret="'+t.secret+'"]'),c=new RegExp("^https?:$","i"),i=0;i<o.length;i++)o[i].style.display="none";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute("style"),"height"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):"link"===t.message&&(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener("message",d.wp.receiveEmbedMessage,!1),l.addEventListener("DOMContentLoaded",function(){for(var e,t,s=l.querySelectorAll("iframe.wp-embedded-content"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute("data-secret"))||(t=Math.random().toString(36).substring(2,12),e.src+="#?secret="+t,e.setAttribute("data-secret",t)),e.contentWindow.postMessage({message:"ready",secret:t},"*")},!1)))}(window,document); </script> https://www.oc.ntu.edu.tw/wp-content/uploads/2024/11/image001.png884489Shou-En Tsao, Po-Yen Shen, Chun-Mao Tseng* The partial pressure of CO2 (pCO2) and CO2 air-sea flux exhibit marked spatial and temporal variability across ocean margins, reflecting the complex interplay of regional environmental processes. Understanding these variations is fundamental to comprehending the global carbon cycle and predicting how oceans may respond to climate change. A recent […]