Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean
We found an implementation error in the calculation of the deposition velocity (vd) which, in turn, affected all the estimated vd-depending parameters (deposition flux, residence time, and traveled distance by microorganisms). Deposition fluxes are now somewhat lower than previously estimated, resul...
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ftcsic:oai:digital.csic.es:10261/318141 2024-02-11T10:06:38+01:00 Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean Mayol, Eva Jiménez, María A. Gerhard, J. Herndl Duarte, Carlos Manuel Arrieta, Jesús María Océan atlantique Atlantic Ocean Océano Atlántico 2017 http://hdl.handle.net/10508/11570 http://hdl.handle.net/10261/318141 https://doi.org/10.3389/fmicb.2017.01971 en eng Centro Oceanográfico de Canarias AM Frontiers in Microbology, 8. 2017: 1-5 http://hdl.handle.net/10508/11570 http://hdl.handle.net/10261/318141 doi:10.3389/fmicb.2017.01971 22553 open Medio Marino Airborne microbes Centro Oceanográfico de Canarias Microbial dispersal Air-Sea Exchange Bioaerosols Atlantic Ocean volume microbiology overturn meteorological data particle size research article 2017 ftcsic https://doi.org/10.3389/fmicb.2017.01971 2024-01-16T11:45:00Z We found an implementation error in the calculation of the deposition velocity (vd) which, in turn, affected all the estimated vd-depending parameters (deposition flux, residence time, and traveled distance by microorganisms). Deposition fluxes are now somewhat lower than previously estimated, resulting in residence times and traveled distances longer than those previously estimated. In addition, the spray fluxes were calculated using a spray generation function (dF/dr0) valid for droplets of radii between 0.5 and 12 μm proposed by Blanchard (1963) and Gathman (1982) as corrected by Andreas et al. (1995). However, in the calculation of dF/dr0, we exceeded this valid range of radii given that we included droplets with radii from 0.2 μm according to the small size of some microbial cells. Thus, a different formulation of dF/dr0, developed by Gong (2003), is now used for the estimation of spray fluxes of microbes, which is valid even for small droplets from a radius of 0.07 μm. Below, we offer a new corrected version of the paragraphs affected by corrections along the text. In addition, we show corrected versions of Figure 1 (forward trajectories according residence times), Figure 3 (deposition velocity values), Figure 5 (spray and deposition fluxes), Figure 6 (Net fluxes), and Table 1. The authors apologize for the errors in the estimates reported in the original manuscript. These corrections only affect the magnitude of some of the reported variables and even though they do not change the scientific conclusions of the article they are reported here for accuracy and reproducibility. SI Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Andreas ENVELOPE(-60.729,-60.729,-64.008,-64.008) Blanchard ENVELOPE(-62.083,-62.083,-64.733,-64.733) Frontiers in Microbiology 8 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Medio Marino Airborne microbes Centro Oceanográfico de Canarias Microbial dispersal Air-Sea Exchange Bioaerosols Atlantic Ocean volume microbiology overturn meteorological data particle size |
spellingShingle |
Medio Marino Airborne microbes Centro Oceanográfico de Canarias Microbial dispersal Air-Sea Exchange Bioaerosols Atlantic Ocean volume microbiology overturn meteorological data particle size Mayol, Eva Jiménez, María A. Gerhard, J. Herndl Duarte, Carlos Manuel Arrieta, Jesús María Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
topic_facet |
Medio Marino Airborne microbes Centro Oceanográfico de Canarias Microbial dispersal Air-Sea Exchange Bioaerosols Atlantic Ocean volume microbiology overturn meteorological data particle size |
description |
We found an implementation error in the calculation of the deposition velocity (vd) which, in turn, affected all the estimated vd-depending parameters (deposition flux, residence time, and traveled distance by microorganisms). Deposition fluxes are now somewhat lower than previously estimated, resulting in residence times and traveled distances longer than those previously estimated. In addition, the spray fluxes were calculated using a spray generation function (dF/dr0) valid for droplets of radii between 0.5 and 12 μm proposed by Blanchard (1963) and Gathman (1982) as corrected by Andreas et al. (1995). However, in the calculation of dF/dr0, we exceeded this valid range of radii given that we included droplets with radii from 0.2 μm according to the small size of some microbial cells. Thus, a different formulation of dF/dr0, developed by Gong (2003), is now used for the estimation of spray fluxes of microbes, which is valid even for small droplets from a radius of 0.07 μm. Below, we offer a new corrected version of the paragraphs affected by corrections along the text. In addition, we show corrected versions of Figure 1 (forward trajectories according residence times), Figure 3 (deposition velocity values), Figure 5 (spray and deposition fluxes), Figure 6 (Net fluxes), and Table 1. The authors apologize for the errors in the estimates reported in the original manuscript. These corrections only affect the magnitude of some of the reported variables and even though they do not change the scientific conclusions of the article they are reported here for accuracy and reproducibility. SI |
format |
Article in Journal/Newspaper |
author |
Mayol, Eva Jiménez, María A. Gerhard, J. Herndl Duarte, Carlos Manuel Arrieta, Jesús María |
author_facet |
Mayol, Eva Jiménez, María A. Gerhard, J. Herndl Duarte, Carlos Manuel Arrieta, Jesús María |
author_sort |
Mayol, Eva |
title |
Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
title_short |
Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
title_full |
Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
title_fullStr |
Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
title_full_unstemmed |
Corrigendum: Resolving the abundance and air-sea fluxes of airborne microorganisms in the North Atlantic Ocean |
title_sort |
corrigendum: resolving the abundance and air-sea fluxes of airborne microorganisms in the north atlantic ocean |
publishDate |
2017 |
url |
http://hdl.handle.net/10508/11570 http://hdl.handle.net/10261/318141 https://doi.org/10.3389/fmicb.2017.01971 |
op_coverage |
Océan atlantique Atlantic Ocean Océano Atlántico |
long_lat |
ENVELOPE(-60.729,-60.729,-64.008,-64.008) ENVELOPE(-62.083,-62.083,-64.733,-64.733) |
geographic |
Andreas Blanchard |
geographic_facet |
Andreas Blanchard |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Centro Oceanográfico de Canarias AM Frontiers in Microbology, 8. 2017: 1-5 http://hdl.handle.net/10508/11570 http://hdl.handle.net/10261/318141 doi:10.3389/fmicb.2017.01971 22553 |
op_rights |
open |
op_doi |
https://doi.org/10.3389/fmicb.2017.01971 |
container_title |
Frontiers in Microbiology |
container_volume |
8 |
_version_ |
1790604471224500224 |