the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
25 Jan 2021
25 Jan 2021
Long distance particle transport to the central Ionian Sea
- 1Aix Marseille Université, Université de Toulon, CNRS, IRD, Mediterranean Institute of Oceanography (MIO), 13288, Marseille, France
- 2Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway
- 1Aix Marseille Université, Université de Toulon, CNRS, IRD, Mediterranean Institute of Oceanography (MIO), 13288, Marseille, France
- 2Department of Arctic and Marine Biology, UiT The Arctic University of Norway, Tromsø, Norway
Abstract. In the upper layers of the Ionian Sea, young Mediterranean Atlantic Waters (MAW) flowing eastward from the Sicily channel meet old MAW. In May 2017, during the PEACETIME cruise, fluorescence and particle content sampled at high resolution revealed unexpected heterogeneity in the central Ionian. Surface salinity measurements, together with altimetry-derived and hull-mounted ADCP currents, describe a zonal pathway of AW entering the Ionian Sea, consistent with the so-called cyclonic mode in the North Ionian Gyre. The ION-Tr transect, located ~19–20° E–~36° N turned out to be at the crossroad of three water masses, mostly coming from the west, north and from an isolated anticyclonic eddy northeast of ION-Tr. Using Lagrangian numerical simulations, we suggest that the contrast in particle loads along ION-Tr originates from particles transported from these three different water masses. Waters from the west, identified as young AW carried by a strong southwestward jet, were intermediate in particle load, probably originating from the Sicily channel. Water mass originating from the north was carrying abundant particles, probably originating from northern Ionian, or further from the south Adriatic. Waters from the eddy, depleted in particles and Chl-a may originate from south of Peloponnese, where the Pelops eddy forms.
The central Ionian Sea hence appears as a mosaic area, where waters of contrasted biological history meet. This contrast is particularly clear in spring, when blooming and non-blooming areas co-occur. Particle abundance in situ measurements are useful to discriminate water masses and derive circulation, together with T-S properties.
Interpreting the complex dynamics of physical-biogeochemical coupling from discrete measurements made at isolated stations at sea is a big challenge. The combination of multi-parametric in situ measurements at high resolution with remote sensing and Lagrangian modeling appears as one proper way to address this challenge.
Léo Berline et al.
Status: final response (author comments only)
-
RC1: 'Comment on bg-2020-481', Anonymous Referee #1, 12 Feb 2021
Review to ms #bg-2020-481
entitled:
“Long distance particle transport to the central Ionian Sea”
By L. Berline et al.
submitted to Biogeosciences.
General comments
The paper examines the heterogeneity observed in the central Ionian Sea with respect to hydrology, productivity and particle properties, using in-situ data collected in 2017 by ship survey as well as remote sensing and Lagrangian modelling data. The sampled biogeochemical and physical data are used to track the various sources and processes that contribute to the marine status of the central Ionian. The manuscript is interesting, however it would benefit by presenting the scope of the research in a more focused way. It is not clear to me if the scope is to show the complexity of the marine environment in the surveyed area or to show different water masses properties and the responsible mechanisms or maybe both.
General comments per Section are listed here below. The use of English is rather good; some “polishing” could be of help. Finally, the ms needs careful editing since there are many minor errors (see Specific comments).
1 Introduction
Since the manuscript aims at focusing on the particle abundance of different water masses in the Ionian Sea, I would like to see a detailed introduction on the importance of studying particle abundance and their dynamics in the world ocean, the Mediterranean Sea, and the Eastern Mediterranean – Ionian Sea in particular. Following that, I believe a listing of methods employed so far to study particle properties should be presented, and then, the authors can present their own methods, combination of methods applied to better describe the particle properties within different water masses.
2 Material and Methods
With respect to the methodological design (Section 2), the authors employed several classic and more advanced instruments/methods to study water mass characteristics and particle properties, resulting in the production of a hefty dataset, rather unique, and certainly not previously available for the Ionian Sea marine area.
3 Results
Results are adequately presented in brief manner (Section 3) and accompanied by a number of well-designed and informative figures. Given that several parameters and measurements are discussed, whilst certain parameters, such as MEP proportion and AI attenuance index are not so common, a moderately lengthier presentation would be beneficial for the reader.
With respect to Section 3.2, I do not think that the full depth T-S diagrams (fig. 6) shown are of any significant use in the ms since observations are focusing on the upper water layers. Consider removing. I would only keep the depth-limited vertical profiles (fig. 7).
The origin of particles presented in section 3.4 is not clear. Particles may be transported as part of water masses circulation, but particles are also introduced locally in the water column via atmospheric precipitation and primary production. Since the scope of the paper is about particles, it would be interesting to differentiate between transported and in situ particle origin. A ‘particle properties signature’ on water masses is a challenge, and I would appreciate if the authors could look deeper into their rich dataset to provide such information, if possible.
In several cases across the document, variable units are following the numerical values without a space (e.g. L171: 70m; L180: 20-90m, etc.). Please check and correct throughout the document. In addition, decimal separator used is sometimes a comma (e.g. L136: 0,09 mg.m-3) or point (e.g. L149: 38.2). Please decide and correct throughout the document. In the same context, units are sometimes given as fractions (e.g. L175 0.3 m/s) or as exponents (e.g. L177: 5 104 #.m-3). Please correct throughout the document.
4 Discussion
The circulation patterns and water mass distribution patterns are presented in the discussion sections 4.1 and 4.2. However, a lot of information seems to fit more nicely at the Results section, and hence should be moved there. That leaves very little a pure discussion to the section. The latter applies also to Section 4.3 on the biological history of water masses. Here, the authors claim that abundant aggregates of diameter larger than 100 μm maybe associated with intense primary production, which, however, does not seem to be the case in the Ionian Sea during the sampling period or some weeks earlier. The authors could consider the presence of Transparent Exopolymer Particles (TEP) as an alternative factor facilitating particle coagulation and thus aggregates formation.
5 Conclusions
This Section briefly summarizes all findings: heterogeneity, water masses origin, particle behavior and implications. What about the initial hypothesis, can we characterize and identify water masses by their particle properties and abundance?
Specific comments:
Abstract: The abstract needs some restructuring. I suggest the last sentence (lines 27-30) could move at the beginning of the abstract. I leave this to authors’ decision.
Line 12 and throughout the text. MAW and AW acronyms are both used for Atlantic water in the ms. Since (mostly in older literature) MAW stands for Modified Atlantic Water and in the ms it stands for Mediterranean Atlantic Water (the latter is not used in literature), I strongly suggest that whenever you refer to Atlantic Water you should use the acronym AW.
Lines 12 and 19: What is “young AW”? Is there an “old AW”?
Line 20: Try replacing the word “intermediate” with another one to avoid confusion with layer-depth meaning. I suggest “moderate” instead.
Line 42: The Ionian Sea (check and correct throughout the manuscript)
Line 55-59: Please provide information regarding station SAV, which appears to be isolated both from other stations and the transect area. Based on what properties was SAV selected?
Line 61: Change “salinity” to “conductivity” which is what the sensor directly reads.
Line 62: State if the fluorometer was calibrated to report chlorophyll-a concentration in mg m-3
Line 63: The primary parameter measured is light transmission (LT, %) and then the beam attenuation coefficient (c, m-1) is estimated according to the path-length (L) of the transmissometer according to: c = -1/L ln(LT/100). Please describe in more detail or give references.
Line 70: WetLabs
Line 78: I cannot find ST8-Tr in figure 1.
Line 70: What is the depth reached by LOPC? Give a range.
Line 85: TSG most probably means ThermoSalinoGraph. Please expand the acronym to its proper meaning.
Line 122: Same as above for SVP.
Line 123: Consider replacing “numerical” with “simulated”. “Numerical particles” sounds a bit strange.
Line 131: Please provide link for the database.
Line 136: Provide value for maximum chlorophyll-a concentration
Line 147: Please provide a range for “low, high” salinity.
Line 159: I do not think that the altimetry shows anticyclonic circulation “across” the basin.
Line 163: Please state that ~0.4°refers to longitude. Same throughout the text.
Line 168: Maybe ‘water mass’ properties
Lines 169-171: This is confusing. You could say that the surface layer which reaches depths up to 30 or 70 m in this or that area, carries a low salinity AW signal, below which salinity increases to more than 39 etc. Please rephrase.
Line 180: terms
Line 186: The density values refer to potential density? Please state in the text. Moreover here and throughout the text density units are missing. Please correct.
Line 196: Replace “carousel” with “CTD”. I do not think that the water sampling at discrete levels from the carouse/rosette can produce continuous profiles as in fig. 7. These are most certainly the product of CTD sensors.
Line 216: Paragraph 3.4 is a bit repetitive. Please restructure.
Lines 261-2-3: I am not sure if the presentation of specific density values here has any particular meaning. Consider omitting.
Line 318: Change “This eddy may have trapped waters from the eastern Ionian, more oligotrophic (Casotti et al 2003),….” to “This eddy may have trapped waters from the more oligotrophic eastern Ionian (Casotti et al 2003),….”.
Line 321: The acronym UVP is used here with no explanation. Please add full meaning: Underwater Video Profiler.
Line 364: Correct 4 to 5
Figure captions:
Fig. 1: What is the difference between full and dotted lines?
Fig. 7: Please add variable names at all x axes
Fig. 8: In the phrase “Black dots are the final positions”, the word “final” possibly refers to the positions of the particles calculated at the beginning of one month before the sampling. If that is true, then “final” should be replaced with “starting” or something similar to avoid confusion.
- AC1: 'Reply on RC1', Leo Berline, 11 May 2021
-
RC2: 'Comment on bg-2020-481', Anonymous Referee #2, 14 Feb 2021
General Comments:
This paper focus on the oceanographic and biological data collected during the PEACETIME cruise in the Ionian Sea in May 2017. The results focus on the heterogeneity of the water masses salinity, fluorescence and particle content observed along the ION-tr transect, suggesting their different origins and connecting them with the surface dynamics of the Ionian Basin. The ION-tr transect results in an interesting crossroads between three different water masses; their presence and characteristics are linked to the basin-scale circulation of the Ionian Sea.
I find this work very interesting and certainly suggest its publication, but I also believe that the authors can still work on improving the description of the context and results. The introduction should be used to explain the importance of this kind of studies and to introduce the dynamics and the surface circulation of the Ionian Sea, in order to give the reader the right elements to better understand and interpret the results. In this form, it becomes very difficult to follow the descriptions without a deep knowledge of the study area. The results of Lagrangian numerical simulation are an important point of this work, and the criteria chosen for the simulations should be explained in more detail.
Specific comments:
Introduction:
I like short, concise introductions, but I find this one too essential. It would be interesting to have a brief discussion of the main results in the literature and some considerations on the importance to study particle distribution.
Lines 47-48: these two sentences seem a repetition.
Lines 51:53: I suggest a broader explanation of the background (PEACETIME cruise) and of the objectives of this study. This sentence rather than explaining the objectives seems to anticipate the results in a cryptic way.
Materials and Methods:
Figure 1: I suggest reproducing the figure in a more accurate way. The transect ST8-tr is not labelled in the figure; the label of the ION-tr transect is positioned away from the transect itself; use different colours for circulation patterns and transects.
Results:
Lines 135-138: Figure 2 is introduced at the beginning of the results without context (it is unclear where the time series was derived from and why). I suggest inserting a paragraph at the beginning of the section that introduces and contextualizes the results explained below. For example, the authors could start by describing the Ionian surface circulation during PEACETIME cruise and explaining why that area was chosen the averages of SST and Chl-a. In the caption of Figure 2, the authors talk about an average on the “northern Ionian Sea”, but actually the selected area involves almost all the Ionian Sea.
Lines 143-144: it should be better explained to the reader how to recognize these cyclonic and anticyclonic structures in Fig. 3a and 3b.
Line 153: this sentence is not clear for me! “Sufficient abundance” of what?
Line 155: add “…of Sicily, where lower salinities are associated to large abundance.”
Line 163: add also a comment about the difference in speeds between AVISO and ADCP currents.
Section 3.3: It would be easier for the reader to follow this description by adding in the text an indication of the sub-plots referred to.
Section 3.4: The results of this figure are essential to understanding the discussions and conclusions sections of this work. For this reason I believe that the authors should explain more accurately what we see in the different panels of Figure 8 and then focus on the results of panels E and F. The rectangle enclosing the location of the ION-tr transect in Figure 8E is really hard to see.
Thecnical Commets:
Line 85: the acronym TSG is not defined
Line 111: check the spatial resolution of the SST.
- AC2: 'Reply on RC2', Leo Berline, 11 May 2021
Léo Berline et al.
Léo Berline et al.
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 305 | 94 | 12 | 411 | 2 | 2 |
- HTML: 305
- PDF: 94
- XML: 12
- Total: 411
- BibTeX: 2
- EndNote: 2
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
