development of tp regional precipitation datasets and products: need and progress
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Development of TP Regional Precipitation Datasets and Products: need and progress. Daqing Yang National Hydrology Research Centre (NHRC) Environment Canada (EC), Saskatoon, Canada Yinsheng Zhang, Yingzhao Ma Institute of Tibetan Plateau Research Chinese Academy of Sciences - PowerPoint PPT PresentationTRANSCRIPT
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Development of TP Regional Precipitation Datasets and Products:
need and progress
Daqing Yang
National Hydrology Research Centre (NHRC)
Environment Canada (EC), Saskatoon, Canada
Yinsheng Zhang, Yingzhao MaInstitute of Tibetan Plateau Research
Chinese Academy of Sciences
3rd TPE Workshop, Sept 1, 2011
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Need for P Data and Products
• Climate: key variable to define climate and its change • Glacier: accumulation and mass balance • Hydrology: flood/drought, water budget, and input to models• Snowcover: mass/energy balance, avalanche• Ecosystem: water supply, NDVI - P relation, vegetation change
vs. precip impact • Human: transportation, recreation, cultural
• 2nd TPE workshop report– 1# product: Precip (when, where, how much, form, and trend) – TPE atlas, i.e. basin/regional hydroclimatology
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Meteorological Stations over TP
• Network: density and distribution
• Data quality:
- space/time discontinuity
- obs biases
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Biases and Correction Method
Pc = K Pg + Pw + Pe + Pt
Pc- corrected precipitation
Pg - gauge-measured precipitation
Pw - wetting loss
Pe - evaporation loss
Pt - trace precipitation
K - correction coefficient for wind-induced undercatch
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Gauge Precipitation
(Yang et al, 1991)Daily Correction Coefficient (K)
Bias-corrected Precipitation
NASA Website TRMM 0.25°3B42_V6 Product
Reliability Evaluation
TRMM Precipitation
Homogenized and correctedPrecipitation
Dataset
FTP Download
DEMPart Ⅱ
Part Ⅰ
Part Ⅲ
Project Flowchart: Homogenized and Corrected Precipitation Dataset over TP
(Goodison et al., 1998)
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WMO Solid Precipitation Measurement WMO Solid Precipitation Measurement Intercomparison, manual and auto gauges Intercomparison, manual and auto gauges
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WMO Double Fence International WMO Double Fence International ReferenceReference
(DFIR) for Solid Precipitation(DFIR) for Solid Precipitation
Secondary reference
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CanadaBarry GoodisonPaul LouieJohn MetcalfeRon Hopkinson
ChinaDaqing YangErsi KangYafen Shi
CroatiaJanja Milkovic
DenmarkHenning MadsenFlemming VejenPeter Allerup
FinlandEsko ElomaaReijo HyvonenBengt TammelinAsko TuominenS. Huovila
IndiaN. Mohan RaoB. BandyopadhyayVirendra KumarCol K.C. Agarwal
GermanyThilo Günther
JapanMasanori ShirakiHiroyuki OhnoKotaro YokoyamaYasuhiro KominamiSatoshi Inoue
NorwayEirik Førland
CRN modified DFIR
• Intercomparison was the result of Recommendation 17 of the ninth session of the CIMO-IX.
• Started in the northern hemisphere winter of 1986/87.
• Field work carried out at 26 sites in 13 Member countries for 7 years
• Final report WMO-TD no. 827 published in 1998
Barry GoodisonChairman, International Organizing Committee
WMO Solid Precipitation Measurement Intercomparisonsites and people
RomaniaViolete Copaciu
Russian FederationValentin GolubevA. Simonenko
SlovakiaMiland Lapin
SwedenBengt Dahlstrom
SwitzerlandBoris SevrukFelix BlumerVladislav Nešpor
UKJ. FullwoodR. Johnson
USARoy BatesTimothy PangburnH. GreenanGeorge LeavesleyLarry BeaverClayton HansonAlbert RangoDouglas EmersonDavid LegatesP. Groisman
WMOKlaus SchulzeStephan Klemm
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Daily catch ratio vs. daily wind speed
CATCH RATIO VS. WIND SPEED, SNOW, DFIR > 3.0mm, 2 WMO SITES
0
20
40
60
80
100
120
140
0 1 2 3 4 5 6 7 8 9
WIND SPEED AT GAUGE HEIGHT (m/s)
NW
S 8
" G
AU
GE
(A
LT
ER
)/ D
FIR
(%
)
Vermont
Valdai
fit
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0
20
40
60
80
100
120
0 1 2 3 4 5 6 7 8 9
Wind speed at gauge height (m/s)
Rat
io o
f gau
ge c
atch
to th
e D
FIR
(%)
Canadian Nipher NWS 8" AlterNWS 8" unsh Hellmann unshTretyakov
WMO Intercomparison Study Results:WMO Intercomparison Study Results:
Catch Efficiency vs. Wind for 4 most widely used Catch Efficiency vs. Wind for 4 most widely used gaugesgauges
Daily time scale Daily time scale
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Barry Goodison, Paul Louie, and Daqing Yang,the 14th Professor Vilho Vaisala Awardin 1998
• About 30 papers in international journals
• National reports
• WMO TD, No- 827, 1998
Report and Publication
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Recommendations from the WMO Intercomparison Study
• WMO correction methods (available for different types of gauges and for different types of precipitation and various time intervals) should be adopted and applied to current and archived data;
• both measured and corrected precipitation data should be reported and archived;
• trace precipitation should be treated as a non-zero event; effort to determine mean trace amount is needed in Arctic conditions;
• additional wind speed measurements be taken at the level of the gauge orifice and hourly mean wind data be archived in order to correct for wind-induced undercatch;
• use of heated tipping-bucket gauges for winter precipitation measurement should be carefully assessed; their usefulness is severely limited in regions where temperatures fall below 0C for prolonged periods of time;
• timing and type of precipitation be recorded by automatic instruments in order to conduct the correction on the basis of precipitation event.
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a) Pm (mm) b) Pc (mm) c) CF
Mean Gauge-Measured (Pm) and Bias-Corrected (Pc) Precipitation, and Correction Factor (CF) for January
-180
-90
0
90
180
45 60 75 90
Pc (mm)
0 - 10
10 - 20
20 - 30
30 - 40
40 - 50
50 - 60
60 - 70
70 - 80
80 - 90
90 - 390
-180
-90
0
90
18045 60 75 90
CF
1 - 1.1
1.1 - 1.2
1.2 - 1.3
1.3 - 1.4
1.4 - 1.5
1.5 - 1.6
1.6 - 1.7
1.7 - 1.8
1.8 - 1.9
1.9 - 2.3
-180
-90
0
90
180
45 60 75 90
Pm (m m )
0 - 10
10 - 20
20 - 30
30 - 40
40 - 50
50 - 60
60 - 70
70 - 80
80 - 90
90 - 330
• Total 4827 stations located north of 45N, with data records longer-than 15 years during 1973-2004.
• Similar Pm and Pc patterns – corrections did not significantly change the spatial distribution.
• CF pattern is different from the Pm and Pc patterns, very high CF along the coasts of the Arctic Ocean.
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Impact of Bias-Corrections on Northern Hydrology: CLM3 simulations with/without P corrections, 1973-04 5~25%
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Annual precip bias-corrections in China, 1951-1998 (Ye et al. 2003, JHM)
80 90 100 110 120 130
20
25
30
35
40
45
50
55
050
100
150
200
300
400500
600
8001000
1200
1400
1600
18002000
2200
2400a. Pm (mm)
80 90 100 110 120 130
20
25
30
35
40
45
50
55
0
50
100
200
400
500
600
800
10001200
1400
1600
1800
2000
2200
2400
2600
2800Corrected annual mean precipitation (mm)China, 1951-98
80 90 100 110 120 130
20
25
30
35
40
45
50
55
b. Pc (mm)
1000
80 90 100 110 120 130
20
25
30
35
40
45
50
55
5
10
15
20
25
30
35
40
45
50
55
60
65
70
75d. (Pc – Pm) / Pm (%)
80 90 100 110 120 130
20
25
30
35
40
45
50
55
0
5
10
25
50
100
150
200
250
300
350
400
450
500
550
600
650 c . Pc - Pm (mm)
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Trend Comparison, measured vs. corrected annual precipitation, 670 stations in China,
1951-98
y = 1.08x - 4.9323R2 = 0.9442
-150
-100
-50
0
50
100
150
-150 -100 -50 0 50 100 150
Trend in measured annual precipitation (mm/10a)
Tre
nd
in
co
rrec
ted
an
nu
alp
reci
pit
atio
n (
mm
/10a
)
a
1:1
y = 0.8938x - 0.5987R2 = 0.9661
-20
-15
-10
-5
0
5
10
15
20
-20 -10 0 10 20
Trend in measured annual precipitation (%/10a)
Tre
nd
in
co
rrec
ted
an
nu
alp
reci
pit
atio
n (
%/1
0a)
b 1:1
Average trend for all stations:
+ 0.5mm/10a for measured precip
- 4.5mm/10a for corrected precip
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Water balance summary for the Yellow river source, 1958-2001
Dataset Runoff (mm)
Precipitation (mm)
Precipitation difference
(%)
Evaporation (P-R) (mm)
Evaporation difference
(%)
Runoff coefficient
Measured 502. 4 0 335.1 0 0.33
Corrected 167. 3 599. 9 19 432.6 29 0.28
EAR-40 171. 5 537. 2 7 365.8 9 0.32
• P = R + E or E = P – R
• P undercatch -> E underestimation ???
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Gauge Precipitation
(Yang et al, 1991)Daily Correction Coefficient (K)
Bias-corrected Precipitation
NASA Website TRMM 0.25°3B42_V6 Product
Reliability Evaluation
TRMM Precipitation
Homogenized and correctedPrecipitation
Dataset
FTP Download
DEMPart Ⅱ
Part Ⅰ
Part Ⅲ
Project Flowchart: Homogenized and Corrected Precipitation Dataset over TP
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Yearly Mean Bias-Corrected Precipitation in TP
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Yearly-Correction Coefficient Distribution in TP
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Sample of TRMM product• weekly accumulation, TRMM-precipitation estimation in Asia,• global 0.25° * 0.25° grid over the latitude band 50°N-S • about seven hours of observation time.
• Key question: TRMM winter data for solid and mixed precip over the mountain regions, i.e. TPE
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Geonor-DF
Bratt’s Lake Intercomparison Facility/Smith
DFIR
Barrow, UAF
DFIR, Mar 3/03
Barrow, UAF Wyoming snow fence, Mar/03 Barrow, UAF DFIR, Mar 03
WMO Solid Precipitation Inter-Comparison
Experiment (WMO-SPICE)
EC Snow Workshop,TorontoDec 01, 2010
Rodica Nitu
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CIMO-XV (Sept 2010)• An instrument intercomparison for solid precipitation measurements at AWS: a
priority!
• WMO-SPICE: WMO Solid Precipitation Instrument Intercomparison Experiment
• Canada committed to a leadership role if other Members participate and share the work
• Support and commitment expressed: China, Finland, Japan, New Zealand, Switzerland, Russian Federation, and USA.
• In CIMO, SPICE positioned in the context of WIGOS, EC-PORS, GCW.
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WMO-SPICE: Proposed objectives
• Evaluate the performance and configuration (catching, non-catching type, instrument & shield) of measurements in field conditions;
• Develop multi-parameter algorithms to improve AWS precipitation data;
• Develop adjustment procedures of systematic errors;
• Establish a field reference standard using automatic gauges;
• Develop long-term capacity to support validation of satellite measurements (e.g. Global Precipitation Measurement);
• Develop comprehensive datasets to support future research objectives;
• Provide feedback to manufacturers;
• Pilot project for WIGOS, EC-PORS, GCW.
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Proposed Ancillary Measurements
• Radar – for horizontal (PPI scans) and vertical profiling (RHI or Vertical scans) for variation of precipitation. Dual-pole for precipitation typing.
• Radiometer – determine the presence of liquid water (determine if particles are rimed).
• Wind measurements (3D anemometers) – for turbulence, gustiness, at sensor height.
• Precipitation Type Sensors – present weather sensors, intensive human observations.
• Temperature and humidity – point and profiling, to determine habit types
• Particle size, particle density and shape information – for aerodynamic collection efficiency issues;
• Snowpack properties – snow depth, snow morphology, snow (freshly fallen and snow pack) density;
• Lidar for cloud properties;
• Upper Air soundings for air mass stability.
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Summary • Large biases/errors in historical gauge precipitation data
• Bias corrections necessary, using WMO methods and station meta data/info
• Impacts of precip bias corrections – changes in max P, mean, variation, and trend– SWE, snowmelt runoff, river flow, water and energy budget
• Needs:– compatibility among gauge observations, manual vs. auto gauges (including TPE networks/stations)– test of auto gauges and instruments – WMO/SPICE– validation of RS P/snowfall data over the cold regions – TPE P working group/project???