The document discusses how the barrier layer off the western coast of Sumatra drastically deepened due to the passage of a Madden-Julian Oscillation (MJO) during the Pre-YMC period. The barrier layer thickness increased from 5m to 60m within one day and up to 85m over five days, which had never been observed before. This drastic deepening was caused by vertical mixing from the MJO forcing and downwelling of the thermocline by an oceanic Kelvin wave occurring in phase with the MJO. High-frequency observations are needed to better understand the ocean's response and role in rainfall formation during MJO events.
Botany krishna series 2nd semester Only Mcq type questions
Drastic change of barrier layer off Sumatra due to MJO passage
1. JAMSTEC/DCOP
Qoosaku MOTEKIQoosaku MOTEKI
Masaki KATSUMATA
Kunio YONEYAMA
Kentaro ANDO
Takuya HASEGAWA
Drastic changeof the barrier layerbarrier layer
off the western coastof Sumatra
due to the MJO passage
during the Pre-YMC
2. light water
heavy water
barrier layer: halocline
depth(m) Salinity(psu)
temperature ( )℃
isopycnic layer depthdepth
isothermal layer depth
ILD( T=0.2 )⊿ ℃
MLD
( [ T=0.2 ])⊿σ ⊿ ℃
3. Drastic deepening of BL
BLT (barrier layer thickness)
increased
from 5m to 60m within 1-day,
up to 85m during 5-days.
Such drastic deepening of BL
has not observed ever.
4. Factors for drastic deepening
BLT increased by
vertical mixing by MJO forcing and
downwelling thermocline
by oceanic Kelvin wave.
in-phase of
MJO and oceanic Kelvin wave
13. light water
heavy water
barrier layer: halocline
depth(m) Salinity(psu)
temperature ( )℃
fresh lens breaking
by vertical mixing
ILD deepening
by Kelvin wave
ILD( T=0.2 )⊿ ℃
MLD
( [ T=0.2 ])⊿σ ⊿ ℃
after MJO
14. Drastic deepening of BL
BLT (barrier layer thickness)
increased
from 5m to 60m within 1-day,
up to 85m during 5-days.
Such drastic deepening of BL
has not observed ever.
15. Factors for drastic deepening
BLT increased by
vertical mixing by MJO forcing and
downwelling thermocline
oceanic Kelvin wave.
in-phase of
MJO and oceanic Kelvin wave
16. BL formation: Salinity stratification tendency
H. adv. V. adv. tilting
stretchin
g vertical mixing
Cronin, M. F., and M. J. McPhaden, 2002: Barrier layer formation during
westerly wind bursts. J Geophys Res-Oceans, 107.
tendency
H. adv. tilting
stretching
vertical mixing
My name is Qoosaku MOTEKI.
I would like to show here the drastic change process of the ocean surface structure by the MJO forcing.
I was on the Research Vessel Mirai cruise to operate this oceanic turbulence observation in December 2015 during the Pre-YMC campaign.
So that’s why I do this study.
First of all, the barrier layer is the difference between the mixed layer depth and isothermal layer depth due to the salinity stratification.
The barrier layer prevent to vertically exchange the heat flux and momentum flux.
So the barrier layer thickness would be one of the key factors for air-sea interaction.
On the basis of the Pre-YMC observations,
BLT increased drastically within only 24 hours during the MJO passage over the R/V Mirai.
Such drastic deepening has not observed ever.
what I want to conclude here is,
Such drastic deepening is due to the vertical mixing by the MJO forcing and downwelling thermocline by oceanic Kelvin wave.
The fact that these two factors in the atmosphere and ocean are in-phase is inducing drastic deepening.
So lets get started with the observed MJO status.
Well-organized MJO convection passed over the eastern Indian Ocean on 13 December in 2015.
taking average of tbb btw 5s-5n, the MJO convection associated with the westerly winds passes during the latter half of the Mirai observation period like this.
Remarkable oceanic response is induced by this MJO forcing of the strong westerly winds...
like this. This is a time-depth cross section of temperature from 3-hourly CTD observation.
Mixed layer depth defined from density difference that is equivalent to 0.2degC is shown by dashed line, and isothermal depth defined from 0.2degC temperature difference is shown by dotted line.
The blue line of the 29degC shows continuous downwelling thermocline from 23 November to 17 December.
Meanwhile, before the MJO arriving on 13 Dec., MLD and ILD are quite shallow and BLT is less than 20 m.
Whereas, as the MJO arriving 13 Dec., ILD is rapidly increasing from 20 m to 80 m, but very shallow MLD is keeping less than 20 m.
Then, BLT is drastically deepening during the MJO passage.
This time lag of deepening of ILD and MLD is due to
very strong salinity stratification near the surface.
Before the MJO, the salinity above 10 m is less than 32 psu that is quite small because of large amount of continuous precipitation everyday.
This strong salinity stratification structure near the surface is called fresh lens.
We clearly find that the fresh lens structure is broken by the MJO forcing after 13 Dec.
So what is the MJO forcing?
This is time-depth cross section of turbulence energy dissipation rate by color.
The bold solid line shows sea surface wind speed with the right axis.
The strong wind peaks of the MJO forcing appear twice on 13 and 15 Dec.
And vertical mixing signals appear as the oceanic response from the MJO forcing.
So this vertical mixing could break the fresh lens structure and the salinity stratification extend downward.
This is one of the factors of the drastic deepening of BLT.
However, vertical mixing signals don’t sufficiently reach up to the bottom of the ILD.
So the downwelling ILD is due to the distinct factor.
That is downwelling Kelvin wave that just arrives Sumatra.
This is time longitude cross section of sea surface height anomaly from ocean objective analysis ECCO2 dataset.
The black contours indicate the surface westerly wind speed from the atmospheric objective analysis.
You can easily see that positive anomaly of sea surface hight under the westerly winds propagates eastward and arrives Sumatra during the Pre-YMC period.
So, as the background, continuous downwelling thermocline during the observation period from 20 m to 100 m is due to the oceanic Kelvin wave.
Above 20 m, there is a remarkable fresh lens structure before the MJO passage, and the fresh lens is broken by the vertical mixing after 13 December due to the MJO forcing.
These two factors induce the drastic deepening of the barrier layer.
That is, the vertical profile with fresh lens structure before the MJO is drastically changed
to this one after the MJO because the fresh lens was broken by the vertical mixing due to the MJO forcing and ILD deepening by oceanic downwelling Kelvin wave.
As a result, a thick barrier layer appears within 24 hours on 13 December.
On the basis of the Pre-YMC observations,
BLT increased drastically within only 24 hours during the MJO passage over.
Such drastic deepening has not observed ever.
what I want to conclude here is,
Such drastic deepening is due to the vertical mixing by the MJO forcing and downwelling thermocline by oceanic Kelvin wave.
The fact that these two factors in the atmosphere and ocean are in-phase is inducing drastic deepening.
Such drastic deepening is due to the vertical mixing by the MJO forcing and downwelling thermocline by oceanic Kelvin wave.
The fact that these two factors in the atmosphere and ocean are in-phase is inducing drastic deepening.
Such drastic deepening is due to the vertical mixing by the MJO forcing and downwelling thermocline by oceanic Kelvin wave.
The fact that these two factors in the atmosphere and ocean are in-phase is inducing drastic deepening.
salinity stratification: vertical derivative of salinity
fluorescence distribution after the MJO shows a trace as a result of vertical mixing
This is time series of mixed layer depth by black, isothermal layer depth by blue, and barrier layer thickness by black dashed line, from 23 Nov. to 17 Dec. based on the CTD observation.
This is time series of mixed layer depth by black, isothermal layer depth by blue, and barrier layer thickness by black dashed line, from 23 Nov. to 17 Dec. based on the CTD observation.
This is time series of mixed layer depth by black, isothermal layer depth by blue, and barrier layer thickness by black dashed line, from 23 Nov. to 17 Dec. based on the CTD observation.
.
Such drastic deepening is due to the vertical mixing by the MJO forcing and downwelling thermocline by oceanic Kelvin wave.
The fact that these two factors in the atmosphere and ocean are in-phase is inducing drastic deepening.