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Diurnal Cycle of Precipitation over the Americas Based on CMORPH

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Diurnal Cycle of Precipitation over the Americas Based on CMORPH. Vernon E. Kousky, John E. Janowiak and Robert Joyce Climate Prediction Center, NOAA. CMORPH (CPC Morphing technique). - PowerPoint PPT Presentation
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Diurnal Cycle of Precipitation over the Americas Based on CMORPH Vernon E. Kousky, John E. Janowiak and Robert Joyce Climate Prediction Center, NOAA
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Page 1: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Vernon E. Kousky, John E. Janowiak

and

Robert Joyce

Climate Prediction Center, NOAA

Page 2: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Uses IR data along with passive microwave data to create global rainfall analyses (60N-60S) at high spatial and temporal resolution.

CMORPH uses IR only as a transport vehicle, i.e. IR data are NOT used to make estimates of rainfall when passive microwave data are not available.

The underlying assumption is that the error in using IR to transport precipitation features is less than the error in using IR to estimate precipitation.

CMORPH (CPC Morphing technique)

Page 3: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Rationale

• Passive microwave (PMW) data provide much better rainfall estimates than IR but these data are spatially and temporally incomplete (instruments on polar- orbiting platforms)

• IR data are abundant both in space & time (polar & geostationary platforms)

• CMORPH combines the superior quality of the PMW-derived precipitation estimates with the excellent sampling characteristics of the IR data

Page 4: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Specifics

• Spatial Grid: 0.0728o lat/lon (8 km at equator)

• Temporal Resolution: 30 minutes

• Domain: Global (60o N - 60o S)

• Period of record: Dec. 2002 – present

Page 5: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Diurnal Cycle of Precipitation: South America

• Computed seasonal mean precipitation (for each 30-minute analysis time plus daily total)

• Computed the seasonal mean percent of total daily rainfall for each 30-minute (48 fields per day) and each 3-hour period (8 per day)

Page 6: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

South America: DJF 2002-2003

Page 7: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Percent Total Precipitation: Diurnal Cycle DJF 2002-03

1 2 3

4 5 6

1 2 3

4 5 6

La Plata Basin

Page 8: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Time-Longitude Section (20-30S) Diurnal Cycle of Precipitation

Nocturnal Maximum just east of the Andes

Afternoon maximum over southern Brazil

Time

Page 9: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Diurnal Cycle DJF 02-03 +

03-04

Page 10: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

South America: DJF 2002-03 2003-04

Page 11: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Time (UTC) of Max. Precipitation: South America – DJF 2002-03

00-03 UTC

00-03 UTC

06-09 UTC06-09 UTC

12-15 UTC

12-15 UTC

18-21 UTC

18-21 UTC

Page 12: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Time (LST) of Max. Precipitation: South America – DJF 2002-03

21-24 LST

20-23 LST

03-06 LST02-05 LST

09-12 LST

08-11 LST

15-18 LST

15-18 LST

Page 13: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Mean Diurnal Cycle: MAM 2003

Day 1

Day 2

Day 3

Day 4

E. Coast

Sea breeze induced convection near the coast on Day 1 propagates westward reaching the western Amazon Basin on Day 3.

W. Coast

Page 14: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Central America/ Mexico: JJA 2003

Page 15: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

United States: JJA 2003

Page 16: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

US/Central Amer./ Mexico: JJA 2003

Page 17: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Conclusion

• The CMORPH precipitation analyses provide the temporal and spatial resolutions necessary to describe the diurnal cycle in precipitation.

• A significant diurnal cycle in precipitation is found over continental regions and even over oceanic areas at some distance from the coasts.

• The diurnal cycle of propagating features, such as the sea-breeze front, is well captured in the CMORPH analyses.

Page 18: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Western Africa: JJA 2003

Page 19: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Southern Africa: DJF 2002-2003

Page 20: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Southeast Asia: JJA 2003

Page 21: Diurnal Cycle of Precipitation over the Americas Based on CMORPH

Indonesia: JJA 2003


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