首页> 外文会议>Proceedings of ESA living planet symposium >APPROPRIATE TREATMENT OF UNCERTAINTY AND AMBIGUITY; A FLEXIBLE SYSTEM FOR CLIMATOLOGICAL CALCULATIONS IN RESPONSE TO AN ON-GOING DEBATE ON THE TRANSFER VELOCITY, K.
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APPROPRIATE TREATMENT OF UNCERTAINTY AND AMBIGUITY; A FLEXIBLE SYSTEM FOR CLIMATOLOGICAL CALCULATIONS IN RESPONSE TO AN ON-GOING DEBATE ON THE TRANSFER VELOCITY, K.

机译:不确定性和不确定性的适当处理;灵活的气候计算系统,可响应传输速度K的持续辩论。

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Air-sea fluxes of gases, including carbon dioxide, arerncommonly calculated using an air-sea flux equation.rnWithin this equation, fluxes are proportional to arntransfer velocity, k. We can use Earth observation or inrnsitu data for the calculation of the fluxes, only if wernadopt a suitable algorithm that typically describes therndependence of k on wind speed and water temperature.rnUnfortunately, appropriate algorithms for the transferrnvelocity of carbon dioxide are debated. Since there is arnlarge body of data, but the perceived information isrncontradictory, more data is unlikely to resolve therndebate swiftly. This ambiguity poses a dilemma forrnestimation of fluxes and their uncertainty. A twofoldrnapproach is adopted. Firstly, we examine critically bothrnalgorithms and outline an alternative more mechanisticrnapproach. Secondly, we construct an open system forrnthe calculation of air-sea fluxes that enables a veryrnbroad range of algorithms to be applied.
机译:通常使用气海通量方程来计算包括二氧化碳在内的气海气通量。在该方程中,气通量与纺丝速度k成正比。仅当采用适当的算法(通常描述k对风速和水温的依赖性)时,我们才可以使用地球观测或原位数据来计算通量。不幸的是,对于二氧化碳的传递速度,人们争论不休。由于存在大量的数据,但是感知到的信息是矛盾的,因此更多的数据不太可能迅速解决。这种歧义性造成通量及其不确定性的两难判断。采用双重方式。首先,我们严格地检查两种算法,并概述另一种更机械的方法。其次,我们构建了一个用于海气通量计算的开放系统,从而可以应用范围很广的算法。

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