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• What is NSST and why NSST analysis?• How does NSST analysis in NCEP GFS work?• Main characteristics of the new scheme• Progress• Experiments & Results• Plan
(a) Night or Day without diurnal warming (b) Day with strong diurnal warming
Near Sea Surface Temperatures (NSST)
)0( == zTTs
rT
rT
sT
wlT
Warm layer
Sub-layerSub-layer
z
TT
)(zTwl
slT
rz
: cannot be observed directly (SST)
: can be observed directly by satellites: IR & MW (sub-layer T-profile)
: can be observed directly by buoys & ships (warm layer T-profile)
: can be observed directly by buoys & ships (reference T)
cz
cz
)(zTsl
rT
)(zTsl
Diurnal warming profile : (0 ~ 4.0K at z=0),Sub-layer cooling profile : (0 ~ 0.8K at z=0),
)(' zTw
)1(~ mmOzc
)5(~ mOzr
z
NSST Profile : )()()( ''zTzTTzT
cwr!+=
)0()(cslzzTzT !<=
)(rrzzTT ==
)0()(rwlzzTzT !<=
)(' zTc
NSST Analysis in NCEP GFS: Components and Interaction
Radiative Transfer Model
(CRTM)
Air-sea Fluxes
AtmosphericModel
(GFS_AM)
in Sub-layer
SST: )0()0( ''
cw
an
rTTT !+
)()( ''zTzTT
cw
an
r!+=
BG:
AtmosphericAnalysis
(GSI)
NSST Analysis
(GSI)
NSST model
)(' zTw
)(' zTc
IC:
rT
zT
!
! )(
rT
zT
!
! )(
)(zTTr!
csl
cb
T
T
,
,
!
!
cbcslTT,,
!
X
Tcb
!
!,
cbTX,
!
)(zTsl
=sT
)()()( ''zTzTTzT
cw
an
r
an!+=
anX
bgX
NSST Analysis in NCEP GFS: Main Characteristics
• NSST is treated as depthdependent– Advantages
• More realistic thermal boundarycondition to atmospheric modeland radiative transfer model
• Short time scale (hours) air-seainteraction included in weatherforecasting
• Diurnal variation in NSSTresolved
– Work• NSST model and its coupling
with GFS_AM• Observation operator and its
Jacobi for the new analysisvariable and NSST data
• Determination of theobservation depth for NSSTdata (satellite, buoys &ships)
• NSST is analyzed within GSI– Advantages
• 6-hourly analysis• Use more types of data easily
– Better data coverage• Assimilate the raw observations
directly– Simpler observation error
• NSST analyzed withatmospheric analysis variables ina single cost function
– Better consistency– Work
• Incorporation of NSST analysisin GSI
• The use of more data: AVHRR,insitu NSST and more
Progress
• A 6-hourly NSST analysis scheme in NCEP GFS has beendeveloped– Boundary condition (SST) for GFS_AM– Boundary condition (sub-layer T-profile) for CRTM
• A series of experiments on this new scheme have beendone and the results are encouraging– Impact of NSST model on CRTM and therefore atmospheric
analysis (reported last year)– Tr analysis with GSI– Impact of NSST model on GFS_AM (7-day forecasting)– Coupled assimilation (parallel run) in preparation
Experiments of Tr analysis in GSI
IR:
MW:
Used in operation+ AVHRR GAC+ NSST of buoys&ships
OCN
Used in operation+ AVHRR GAC+ NSST of buoys&ships
CTL
Lower thermal boundarycondition to CRTM
Analysisvariable
Observation Data
)()( ''
ircirw
bg
r zTzTT !+
)(' mww
bg
r zTT +
bgSST
rT
SST
)(),( ''zTzT
cw : Provided by uncoupled NSST model (forced byavailable NCEP 3-hourly operational fluxes)
Experiment period: 09/01/2007 ~ 09/07/2007
:
:
!"
#$%
&
'
'(
'
'))*
+,,-
.(
'
'=
s
Q
s
r
r
h
r
sw
rpo T
I
T
z
z
I
z
I
zcW
/
2
0
!"
#$%
&
'
'+
'
'(()
*++,
-
'
'.=
s
Q
s
r
r
sw
r
h
rpo
dT
I
T
z
z
I
z
I
zcW
22
2/
!"
#$%
&
'
'((+
'
'=
s
cccnscc
s
cT
zzARSQ
T
QzC )(
10 )
*
!!"
#$$%
&
'
'(
'
'=
ss
ccnscd
T
Q
T
zARC )
*
1
Sensitivities of T(z) to Tr
czz !!0z
CW
CW
CWT
Tdd
r
z
000011
1
+!
!+
+!=
"
"
rczzz !!z
CW
W
CW
C
T
Td
r
z
0000
0
11
1
+!+
+!
+=
"
"
GDAS analysis (00Z, 06Z, 12Z, 18Z)OCN
GDAS analysis (00Z, 06Z, 12Z, 18Z)CTL
GFS analysis (00Z, 06Z, 12Z, 18Z)GFS
SSTAtmospheric
Initial Conditions
opSST
opSST
)0()0( ''
cw
opTTSST !+
)0()0( ''
cw
opTTSST !+
'',cwTT
: NCEP operational SST analysis
: Provided by coupled model (GFS_AM + NSST model)
Experiments of NSST model on GFS 7-day forecasting.
The experiments (CTL and OCN) have been done for 3 months:July 2007. January 2008 and September 2007.