the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Synoptic-intraseasonal variability control on high chlorophyll-a events in the Puyuhuapi Fjord, Chilean Patagonia
Reynier Bada-Diaz
Martín Jacques-Coper
Laura Farías
Diego Narváez
Italo Masotti
Abstract. Intraseasonal climate variability as, the Madden-Julian Oscillation (MJO), and synoptic-scale systems modify the normal conditions of the atmosphere and ocean, causing anomalies in sea surface temperature (SST) and salinity (S) which could create an environment conducive to algal bloom events in fjord systems, which in some cases can be toxic (HABs). In this work, an analysis of the atmospheric forcings on the synoptic-to-intraseasonal scale (SY-IS), that precede and proceeds to extreme high chlorophyll-a (chl-a) events was made in the Puyuhuapi fjord (44.7º S 72.8º W), during the summer season (December–February, DJF) between the years 2010–2018. Extreme events of high chl-a are defined when chl-a anomalies exceed the 90th percentile, and day 0 was defined as the maximum anomalous value. Six extreme events, corresponding to 83 % of the total, were detected in the year 2016, a year with strong El Niño southern Oscillation (ENSO). From the analysis of the SY-IS patterns of persistent atmospheric anomalies during these 2016 events and their similarities, we detected that 4 events presented the characteristic of the passage of a low-pressure system, starting at least 7 days before the extreme chl-a event, with negative anomalies of sea level pressure and surface temperature, a change in wind direction and an increase in salinity at surface waters. we propose an atmospheric-oceanographic mechanism that induces favourable conditions for high phytoplanktonic activity in summertime: the passage of a low-pressure system, that weakens stratification and induces upwelling of deeper, colder and nutrient-rich waters favouring an increase in phytoplankton activity and the occurrence of extreme events of high chl-a in Puyuhuapi fjord. Furthermore, this work suggests that active phases 6 and 7 of the MJO might reinforce, on the SY-IS time scale, in DJF 2016. In the case of microalgae blooms, in addition to the well-known seasonal and interannual behaviors, it is important to superimpose the high-frequency variability. To improve the predictive ability of algal blooms and their relationship with climate conditions is essential for managing and mitigating their negative impacts on aquatic ecosystems, human health, and the economy.
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Reynier Bada-Diaz et al.
Status: open (until 07 Dec 2023)
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RC1: 'Comment on egusphere-2023-2272', Anonymous Referee #1, 13 Nov 2023
reply
Review of "Synoptic-intraseasonal variability control on high
chlorophyll-a events in the Puyuhuapi Fjord, Chilean Patagonia" by
Bada-Diaz et al., submitted to Ocean Science.Recommendation: reject.
This paper documents the occurrence of extreme events in chl-a in the
Puyuhuapi Fjord system in Chile and relates them to atmospheric
forcing in an attempt to find an atmospheric causal relationship. The
methodology appears sound. However, the interpretation, that the chl-a
events are caused by the MJO is not supported by the data.MAJOR COMMENTS
1. The number of extreme chl-a events in the study is too low to base
any reliable statistical conclusion on. Also, it is not clear how many
events there actually are. In the abstract, it is stated that 6 (83%)
of the extreme events occur in 2016. This would imply 7
events. However, in table 4, there are only 6 events listed in total
(with 3 of these in (December) 2016). So it is not clear how many
events there are, but either 6 or 7 is far too small a number to base
any reliable conclusions on.2. Of the 6 high chl-a events listed in Table 4, the MJO phases are
also listed. These are, for the 6 events, MJO phases 4,6,7,2,6,5. In
the abstract, it is concluded that MJO phases 6-7 tend to reinforce
chl-a events. This is an incorrect conclusion. 3 out of 6 of the high
chl-a events occur in MJO phases 6-7. With such a small number of
events, and no prior reason to think that MJO phases 6-7 re important,
this can easily happen by pure chance. Also, it is stated that ENSO
is an important modulator of the high chl-a events, as 2016 is an ENSO
year. The paper only analyses DJF data, and it is not clear whether
the 2015/16 or 2016/17 DJF season is being discussed, which is very
confusing. What is the state of ENSO in these two DJF seasons. The
whole discussion here is confusing and not backed up reliably by the
data.Citation: https://doi.org/10.5194/egusphere-2023-2272-RC1
Reynier Bada-Diaz et al.
Reynier Bada-Diaz et al.
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