potential predictability of seasonal mean river discharge in dynamical ensemble prediction using...
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![Page 1: Potential predictability of seasonal mean river discharge in dynamical ensemble prediction using MRI/JMA GCM Tosiyuki Nakaegawa MRI, Japan](https://reader036.vdocument.in/reader036/viewer/2022062802/56649e985503460f94b9b792/html5/thumbnails/1.jpg)
Potential predictability of seasonal mean river
discharge in dynamical ensemble prediction using
MRI/JMA GCM
Tosiyuki NakaegawaMRI, Japan
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Background
• Dependable seasonal predictions would facilitate the water resources managements.
( Nakaegawa et al.2003 )
GMT Jun 6 15:32:35 2002Tosi
0û 60û 120û 180û 240û 300û-90û
-60û
-30û
0û
30û
60û
90û
0.0 0.2 0.4 0.6 0.8 1.0
P-E Variance Ratio JJAJJA MJ98
Cont. Int. = 0.2 [Nodim.]
• Potential predictability of potentially available water resources (P-E) is low in most of land areas.
Are there any factors in improving the predictability?
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Physical characteristics of river discharge
• River discharge is a collection of total runoffs in an upper river basin, which is similar to the area average process.
The collection is likely to reduce the unpredictable variability and, as a result, to enhance the predictability.
P-E: each grid
River discharge: accumulation
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Objectives
•Estimation of the potential predictability of river discharge based on an ensemble experiment
•Examination of the effects of land surface hydrological processes on the predictability, in comparison with that of P-E.
The collection effect
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C20C Experiment setup• AGCM: MJ98 , T42 with 30 vertical layers
• River Routing Model: GRiveT, 0.5o river channel network of TRIP, velocity: 0.4m/s
• Member: 6• SST & Sea Ice : HadISST (Rayner et al. 2003)
• CO2 : annualy varying
• Integration period: 1872-2005
• Analysis period : 1951-2000
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Potential Predictability
• Definition: The maximum value that an ensemble approach can reach, assuming that perfectly predicted SSTs are available and that the model perfectly reproduces atmospheric and hydrological processes.
• Variance ratio : measure of
PP based on the ANOVA
(Rowell 1998).222
222
22
/
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INTSSTTOT
INTEMSST
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Variance Ratio of Seasonal Mean River Discharge
•High in Tropics and Low in Extratropics and inland areas•Seasonal cycles in both Tropics and ExtratropicsHigh for JJA; high for DJF
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Variance Ratio of Seasonal Mean River Discharge
•Resemblance of geographical distributions of the variance ratios of precipitation and P-EA major factor in the predictability of river discharge
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Variance Ratio in the Amazon River Basin
Runoff collection through a river channel network may enhance the variance ratio.
higher variance ratios along major stream channels
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Latitudinal distribution of variance ratios
○ : Variance ratio at river mouths of basins larger than 105km2
Solid line: Zonal mean of the variance ratio of P-E over land areas
Discharge>P-E P-E> Discharge
P-E for DJF > P-E for JJA
Weak
Strong
WeakThe magnitude relation varies with season.
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Collection Effect
• How much influence does the collection effect over a river basin have on the potential predictability of river discharge?
Variance Ratio: (Discharge)-(P-E)
ImprovementBasin areas >106km2Does not work effectively
Cause deterioration
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Relationship between morphometric properties and discharges
• Morphometric properties change the precipitation-discharge responses for basins with the same drainage area (Jones, 1997).
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Variance Ratio Difference and Morphometirc Properties
Total Length
Mainstream Length
Form Factor
Drainage Density
L/A
L2/AL
Absolute properties Relative properties
The size of a river basin influences the collection effects.
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The Amazon River
Discharge
P-E
Impr
ovem
ent
P-E
Discharge
Red
ucti
on
Amazon River
Mean travel time
Madeira: 86 days
Xingu: 45 days
M
X
A
Semi-annual cycle
Month
Var
ianc
e R
atio
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The Mackenzie River
Impr
ovem
ent
The peak of the variance ratio
River discharge: MAM; P-E: DJF
The mean travel time: 68 days
P-E: accumulated as snow in winter and melted in spring
P-E
Discharge
Var
ianc
e R
atio
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The Ob River
Impr
ovem
ent
The peak of the variance ratio
River discharge: JJA; P-E: SON
The mean travel time: 68 days
River discharge in JJA mostly originates from snow melt water, not from P-E.
P-E
Discharge
Var
ianc
e R
atio
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Further Experiment
Further experiment: slower velocity v=0.14m/s(Hagemann and Dumenil 1998)
v=0.14m/s
v=0.40m/s
The collection effects:•Improvement •Phase shift, and •Smoothing
0.2
50
.15
smoothed
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Concluding Summary (1)
• Estimation of the potential predictability of river discharge based on an ensemble experiment with the C20C setup.
Similar geographical distribution to P-E•High in Tropics and low in extratropics and in inland areas
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Concluding Summary (2)
Snow processes significantly influences on the predictability for the mid- and high latitude river basins.Snow accumulation and snow-melting
Distinctive collection effects are identified in large basins with greater than 106km2.Improvement in the variance ratio, phase shift, and smoothing
• Examination of the effects of land surface hydrological processes on the predictability, in comparison with that of P-E.