期刊
ATMOSPHERIC CHEMISTRY AND PHYSICS
卷 18, 期 6, 页码 4297-4315出版社
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-18-4297-2018
关键词
-
资金
- NIWA's Atmosphere Research Programme
- US NSF Atmospheric Chemistry [0851407, 0851472, 1143709]
- IR/D programmes
- Norwegian Research Council [233901, 244262]
- Science Foundation Ireland [16/TIDA/3916]
- Irish Marine Institute [PBA/ME/16/01]
- UK NERC [NE/N018095/1]
- Natural Environment Research Council [pml010009, pml010002, pml010007, NE/P021409/1] Funding Source: researchfish
- Science Foundation Ireland (SFI) [16/TIDA/3916] Funding Source: Science Foundation Ireland (SFI)
- NERC [NE/P021409/1, pml010007, NE/N018095/1, pml010002, pml010009] Funding Source: UKRI
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [1143709] Funding Source: National Science Foundation
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [0851407] Funding Source: National Science Foundation
Parameterisation of the air-sea gas transfer velocity of CO2 and other trace gases under open-ocean conditions has been a focus of air-sea interaction research and is required for accurately determining ocean carbon uptake. Ships are the most widely used platform for air-sea flux measurements but the quality of the data can be compromised by airflow distortion and sensor cross-sensitivity effects. Recent improvements in the understanding of these effects have led to enhanced corrections to the shipboard eddy covariance (EC) measurements. Here, we present a revised analysis of eddy covariance measurements of air-sea CO2 and momentum fluxes from the Southern Ocean Surface Ocean Aerosol Production (SOAP) study. We show that it is possible to significantly reduce the scatter in the EC data and achieve consistency between measurements taken on station and with the ship underway. The gas transfer velocities from the EC measurements correlate better with the EC friction velocity (u(*)) than with mean wind speeds derived from shipboard measurements corrected with an airflow distortion model. For the observed range of wind speeds (u (10) (N) = 3-23 m s(-1)), the transfer velocities can be parameterised with a linear fit to u(*). The SOAP data are compared to previous gas transfer parameterisations using u (10) (N) computed from the EC friction velocity with the drag coefficient from the Coupled Ocean-Atmosphere Response Experiment (COARE) model version 3.5. The SOAP results are consistent with previous gas transfer studies, but at high wind speeds they do not support the sharp increase in gas transfer associated with bubble-mediated transfer predicted by physically based models.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据