Operational Monitoring of Trace Gases over the Mediterranean Sea

<div>Mesh surface of <svg height="11.6478pt" id="M124" style="vertical-align:-3.051061pt" version="1.1" viewbox="-0.0498162 -8.59674 9.65096 11.6478" width="9.65096pt" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><g transform="matrix(.013,0,0,-0.013,0,0)"><path d="M434 650H168L162 618C248 609 258 608 243 528L174 155C163 93 153 39 138 1C110 -68 67 -98 24 -111L37 -147C55 -144 75 -136 94 -128C185 -87 232 -12 259 139L328 528C342 605 349 609 427 618L434 650Z" id="g50-75"></path><glyph.data ascent="3443" descent="-2856" horiz-adv-x="458" vert-adv-y="458"></glyph.data></g><g transform="matrix(.0091,0,0,-0.0091,5.07,3.001)"><path d="M418 650H141L133 618C225 611 232 604 218 531L141 120C126 45 119 37 33 32L24 0H301L308 32C220 37 214 44 227 120L305 531C319 605 325 611 411 618L418 650Z" id="g50-74"></path><glyph.data ascent="3443" descent="-2856" horiz-adv-x="442" vert-adv-y="442"></glyph.data></g></svg>. The Jacobian derivative of the interferogram radiance with respect to the mixing ratio profile of CO.</div>

Advances in Meteorology

Operational Monitoring of Trace Gases over the Mediterranean Sea

Figure 3