The influence of short-term variability in surface water on modelled air–sea exchange

A. Lansø, L. Sørensen, J. Christensen, A. Rutgersson, C. Geels
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引用次数: 2

Abstract

Coastal seas and estuarine systems are highly variable in both time and space and with their heterogeneity difficult to capture with measurements. Models are useful tools in obtaining a better spatiotemporal coverage or, at least, a better understanding of the impacts such heterogeneity has in driving variability in coastal oceans and estuaries. A model-based sensitivity study is constructed in this study in order to examine the effects of short-term variability in surface water p on the annual air–sea exchange in coastal regions. An atmospheric transport model formed the basis of the modelling framework for the study of the Baltic Sea and the Danish inner waters. Several maps of surface water p were employed in the modelling framework. While a monthly Baltic Sea climatology (BSC) had already been developed, the current study further extended this with the addition of an improved near-coastal climatology for the Danish inner waters. Furthermore, daily surface fields of p were obtained from a mixed layer scheme constrained by surface measurements of p (JENA). Short-term variability in surface water p was assessed by calculating monthly mean diurnal cycles from continuous measurements of surface water p, observed at stationary sites within the Baltic Sea. No apparent diurnal cycle was evident in winter, but diurnal cycles (with amplitudes up to 27 atm) were found from April to October. The present study showed that the temporal resolution of surface water p played an influential role on the annual air–sea exchange for the coastal study region. Hence, annual estimates of exchanges are sensitive to variation on much shorter time scales, and this variability should be included for any model study investigating the exchange of across the air–sea interface. Furthermore, the choice of surface p maps also had a crucial influence on the simulated air–sea exchange.
地表水的短期变率对模拟海气交换的影响
沿海海和河口系统在时间和空间上都是高度可变的,它们的异质性很难用测量来捕捉。模式是获得更好的时空覆盖的有用工具,或者至少是更好地了解这种异质性在推动沿海海洋和河口变率方面的影响。为了考察地表水p的短期变化对沿海地区年海气交换的影响,本文构建了一个基于模型的敏感性研究。一个大气输送模式构成了研究波罗的海和丹麦内水的模式框架的基础。在建模框架中使用了几个地表水p图。虽然已经编制了每月一次的波罗的海气候学(BSC),但目前的研究进一步扩大了这一范围,增加了改进的丹麦内水域近岸气候学。此外,由表面测量p (JENA)约束的混合层方案获得了p的日表面场。通过计算在波罗的海固定站点观测到的地表水p连续测量的月平均日循环,评估了地表水p的短期变化。冬季无明显的日循环,但4 - 10月有明显的日循环(振幅可达27 atm)。研究表明,地表水p的时间分辨率对沿海研究区年海气交换具有重要影响。因此,年交换估计值对更短时间尺度上的变化很敏感,任何调查海气界面交换的模式研究都应包括这种变率。此外,地表p图的选择对模拟的海气交换也有重要影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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