Abstract

In situ measurements representing the marine atmosphere and air–sea interaction are taken at ships, buoys, stationary moorings and land-based towers, where each observation platform has structural restrictions. Air–sea fluxes are often small, and due to the limitations of the sensors, several corrections are applied. Land-based towers are convenient for long-term observations, but one critical aspect is the representativeness of marine conditions. Hence, a careful analysis of the sites and the data is necessary. Based on the concept of flux footprint, we suggest defining flux data from land-based marine micrometeorological sites in categories depending on the type of land influence: 1. CAT1: Marine data representing open sea, 2. CAT2: Disturbed wave field resulting in physical properties different from open sea conditions and heterogeneity of water properties in the footprint region, and 3. CAT3: Mixed land–sea footprint, very heterogeneous conditions and possible active carbon production/consumption. Characterization of data would be beneficial for combined analyses using several sites in coastal and marginal seas and evaluation/comparison of properties and dynamics. Aerosol fluxes are a useful contribution to characterizing a marine micrometeorological field station; for most conditions, they change sign between land and sea sectors. Measured fluxes from the land-based marine station Östergarnsholm are used as an example of a land-based marine site to evaluate the categories and to present an example of differences between open sea and coastal conditions. At the Östergarnsholm site the surface drag is larger for CAT2 and CAT3 than for CAT1 when wind speed is below 10 m/s. The heat and humidity fluxes show a distinctive distinguished seasonal cycle; latent heat flux is larger for CAT2 and CAT3 compared to CAT1. The flux of carbon dioxide is large from the coastal and land–sea sectors, showing a large seasonal cycle and significant variability (compared to the open sea sector). Aerosol fluxes are partly dominated by sea spray emissions comparable to those observed at other open sea conditions.

Highlights

  • The surface of the Earth is dominated by oceans

  • Category 2 (CAT2): Coastal sea, a local wave field influenced by bathymetry or limited fetch, resulting in physical properties different from open sea conditions or strong gradients of temperature and salinity in the footprint region due to the water depth

  • In the eastern CAT2 sector we observed a stronger contribution from sea spray emissions than from the Category 1 (CAT1) sector, suggesting that shallow water influence on the wave breaking enhanced sea spray formation

Read more

Summary

Introduction

Covering ca 70% of the area, oceans as well as air–sea interaction are important components in any global modelling system. About 7% of the world ocean area can be defined as coastal regions (Gattuso et al, 1998). Marginal seas and coastal areas are key areas in the global carbon cycle, as they support a significant portion of the global primary productivity and draw a substantial flux of atmospheric CO2 into the ocean (Chen et al, 2013). Muller-Karger et al (2005) estimated that the shelf seas might be responsible for as much as 40% of the global oceanic carbon. This article has been republished with minor changes. These changes do not impact the academic content of the article

Methods
Findings
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call