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1 ______ _ Yanping Li Convection - permitting WRF regional climate simulations over Western Canada

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Page 1: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

11______ _Yanping Li

Convection-permitting WRF regional climate simulations over Western Canada

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Available RCM output for CCRN regionCRCM5 CanRCM4 NACCAP CCRN-WRF

Spatial Resolution

50 km NAM-22 (25 km)

NAM-44 (50 km)

50 km 4 km

Vertical levels 29 4 26 51

Temporal resolution

daily NAM-22(daily)

NAM-44(daily, hourly for Pr)

3-hourly hourly

Downscale from CanESM2 CCCma-CanESM2 11 members CMIP5 models 20 ensemble

Scenario RCP4.5, RCP8.5 RCP4.5, RCP8.5 SRES A2 RCP8.5

Output available

2006-2100 1950-2005 (historic)

2006-2010 (future)

1971-2000 (historic)

2041-2070 (near future)

2000-2013 (historic)

2086-2099 (PGW equivalent)

CRCM5 NACCAP CCRN-WRF

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WRF Model Setup and Design WRF Model (Version 3.4.1)

A single domain: 2560 x 2800 km2;

4 km grid spacing; 37 levels

Microphysics Scheme: New Thompson et al.

PBL scheme: YSU

RRTMG Long-wave and Short-wave scheme

No Cumulus parameterization used, assumed explicit

Forcing Data The 6-hourly, 0.7030 x 0.7030

resolution ERA-Interim reanalysis data provide the initial and lateral boundary condition

Continental Scale Regional Climate Simulation using 4-KM WRF

MRB

SRB

MRB: Mackenzie River BasinSRB: Saskatchewan River Basin

NCAR CONUS domain

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Historical simulation (CTRL)

Future simulation (PGW)WRF Dynamical downscaling and

PGW method

DYNAMICAL

DOWNSCALING

HINDCAST

DYNAMICAL DOWNSCALING FUTURE PGW

Weather Research Forecast V3.6

HIGH-RESOLUTION (4-km) REGIONAL CLIMATE

MODEL

PSEUDO GLOBAL WARMINGERA-I + ΔCIMP5

Global monthly multi-model average increments:ΔCIMP5 = projection ensemble − historical ensemble

(2070 to 2099) (1976 to 2005)

RCP8.5 “the business as usual” scenario projectsa 3.7oC warming by the end of the 21 century.

GLOBAL

FUTURE

SCENARIOS ACCESS1-3CanESM2CCSM4CESM1-CAM5CMCC-CMCNRM-CM5CSIRO-Mk3-6-0

CMIP5 models under

RCP8.5GFDL-CM3GFDL-ESM2MGISS-E2-HHadGEM2-CCHadGEM2-ESInmcm4

IPSL-CM5A-MRMIROC5MIROC-ESMMPI-ESM-LRMPI-ESM-MRMRI-CGCM3

6-hours historical boundary conditions from:ERA-Interim reanalysis (ERA-I)

•Sea surface temperature and ice •Air temperature •Horizontal wind

OBSERVATION

PERIOD 2001-2015

• Specific humidity• Air pressure • Geopotential height

Page 5: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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WRF dynamical downscaling for 2000-2013

CMIP5-historic WRF-historic CMIP5-historic WRF-historic

Winter

Spring

Summer

Fall

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Annual precipitation – CMIP5 vs WRF

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WRF dynamical downscaling of CMIP5WRF-PGW WRF-PGW

Winter

Spring

Summer

Fall

WRF-historic WRF-historic

Page 8: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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Daily Tmin

Daily Tmax

Geographic distribution of seasonal mean precipitation (a), Tmin (b) and Tmax (c), over the period from Oct 2000 – Sept 2013 for WRF and ANUSPLIN.

Page 9: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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Monthly T2: CONUS-WRF CCRN-WRF

Jan Feb Mar

Apr May Jun

Jul Aug Sep

Oct Nov Dec

Jan Feb Mar

Apr May Jun

Jul Aug Sep

Oct Nov Dec

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Monthly PR: CONUS-WRF CCRN-WRF

Jan Feb Mar

Apr May Jun

Jul Aug Sep

Oct Nov Dec

Jan Feb Mar

Apr May Jun

Jul Aug Sep

Oct Nov Dec

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CONUS-WRF precipitation validation

Page 12: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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CCRN-WRF Performance Evaluation (Annual cycle)

SRB

MRB

ANUSPLINNARRWRFCaPA

T T

T

T

P

P

P

P

Page 13: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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WRF Precipitation Annual cycle for SRB

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WRF Temperature Annual cycle for SRB

Page 15: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

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MRB

SRB

PR T2

Precipitation, Temperature Annual cycle for MRB, SRB

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SRB

CCRN-WRF Performance Evaluation -PDF for daily precipitation intensity

MRB

Log

X &

Lo

g Y

L

ine

ar X

& L

og

Y

Log

X &

Lo

g Y

L

ine

ar X

& L

og

Y

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CCRN-WRF Performance Evaluation -PDF for hourly precipitation intensityFr

eq

ue

ncy

MRB SRB

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CCRN-WRF Performance Evaluation (Diurnal cycle)

Temperature (oC)

MRB SRB

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WRF Domain –CCRN + CONUS & Extended GWF

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Sensitivity test for land-atmosphere interaction

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WRF NDOWN

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2121

Using 4-km WRF CONUS simulations to diagnose surface coupling strength

Page 22: Atmospheric Dynamics that Condition Extreme Precipitation ... · MRB SRB PR T2 Precipitation, Temperature Annual cycle for MRB, SRB. 16 SRB CCRN-WRF Performance Evaluation-PDF for

2222Lucia Scaff, D. Yang, Yanping Li*, E. Mekis, 2015: Inconsistency in precipitation measurements across Alaska and

Yukon border, The Cryosphere, 9, 2417-2428, 2015.

Precipitation measurements across Canada-US border

Lucia Scaff PhD Student

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Xicai Pan, Daqing Yang, Yanping Li*, Alan Barr, Warren Helgason, Masaki Hayashi, Philip Marsh, John Pomeroy, Richard Janowicz, 2016:Bias Corrections of Precipitation Measurements across Experimental Sites in Different Ecoclimatic Regions of Western Canada, The Cryosphere, 10, 2347-2360

Bias Corrections of Precipitation measurements across different ecoclimate regions

Xicai PanPDF