SERVICIO  NACIONAL DE METEOROLOGIA E  HIDROLOGIA SENAMHI ABRIL, 2010 Analysis of extreme rainfall in Cusco in  Summer 2010 Ing. Jorge Chira La Rosa [email_address] PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
Introduction Analysis of the rainfall episode Conclusions Recommendations SUMMARY PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
An extreme precipitation event that affected almost all south highland of Peru is investigated. This event caused very strong socioeconomic impacts in the Cusco region.   The outstanding event of 22–24 January 2010 was connected to a strong south-esterly flow, probably caused by a intensity of  South Atlantic convergence zone  that persisted for several days and brought unusually large levels of moisture to the South Peru . INTRODUCTION PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
Satellite Pictures-TERRA-Modis January 21, 2010 Source: INPE/CPTEC/BRASIL
Pictures Animation-GOES Satélite  January 21-25, 2010 Source: INPE/CPTEC/BRASIL
Study Area The city of  Cusco  is located at the central and south-eastern zone of Peru, Near Cusco is Vilcanota/Urubamba River valley. located about 10 miles north of Cusco Peru, and extends northwest through Pisac and Ollantaytambo cities. Manned weather stations in Cusco. Just three automatic weather stations in this place.
Rainfall Distributión  Vilcanota River Basin Source: DCL/SENAMHI The rainfall incress between January 21-25 along the basin. High Basin Low Basin Medium Basin
Historical Rainfall in January Pisac-Cusco The picture shows a high amount of rainfall in january, 2010
Strong flow of Vilcanota river in Pisac, Cusco with  327 m3/s top exceed its historical values. Strong Flow of Vilcanota River of  Cusco
Source: Civil Defense Institute Rainfall Impacts in South Peru
Source: Red Cross Flood Impacts in South Peru
Flood Impacts in Cusco city
Damage caused by floods in  Cusco Source:  EL COMERCIO Newspaper ( February 08, 2010) Deads   9 Injured people   10 Homes affected  10.325 Schools afected 35 Medical center affected 06 People affected 21.393 Losses  4 Homes destroyed 4.828 Schools destroyed 9 Medical center  destroyed 02 Churchs affected 15 Public places affected  143 (losas, parques, estadios y otros) Losses (millions de US dolars)  250 Destroys railroads   6,15 km Affected railroads    2,45 km  Asphalt roads  destroyed  18 km  Unpaved Road destroyed    11 km Track roads destroyed  56 km Track bridges destroyed    21  Track bridges affected    30 Fallen street light  477 Losen water intake    86  Farms destroyed  (Ha)  16.281 Farms Affected  (Ha)   10.950
| WARNING ISSUE
This figure shows the CLIMATE OUTLOOK issued to media, decision makers and stakholders before event Climate Forecast of Rainfall  December 2009- February 2010 Extreme rainfall
During January 2010 heavy rainfall affected south Peru, increase of river and floods in Cusco, especially in Pisac city. We observe incress activity of South Atlantic convergence zone  that persisted for several days and brought unusually large levels of moisture to the South Peru. The good cooperation between SENAMHI, Civil Defense Institute and Economy Ministry, lead to finance one automatic weather station loosen during this unusual floods. At this moment there are a project supported by national government to deploy 12 automatic weather station in that place. This project was designed before this event. CONCLUSIONS
To establish an Early Warning System is neccesary in Cusco region, to warning the population by natural disaster. To strengthen  the capacity of local civil defense teams and organizations is necesary.  To organize the population is requerid to improve the emergency management. Disaster Risk Management Specialists is necesary in order to manage the emergency and prevent future risks. RECOMMENDATIONS

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Cusco heavy rainfall

  • 1. SERVICIO NACIONAL DE METEOROLOGIA E HIDROLOGIA SENAMHI ABRIL, 2010 Analysis of extreme rainfall in Cusco in Summer 2010 Ing. Jorge Chira La Rosa [email_address] PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
  • 2. Introduction Analysis of the rainfall episode Conclusions Recommendations SUMMARY PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
  • 3. An extreme precipitation event that affected almost all south highland of Peru is investigated. This event caused very strong socioeconomic impacts in the Cusco region. The outstanding event of 22–24 January 2010 was connected to a strong south-esterly flow, probably caused by a intensity of South Atlantic convergence zone that persisted for several days and brought unusually large levels of moisture to the South Peru . INTRODUCTION PERÚ Ministerio del Ambiente Servicio Nacional de Meteorología e Hidrología - SENAMHI
  • 4. Satellite Pictures-TERRA-Modis January 21, 2010 Source: INPE/CPTEC/BRASIL
  • 5. Pictures Animation-GOES Satélite January 21-25, 2010 Source: INPE/CPTEC/BRASIL
  • 6. Study Area The city of Cusco is located at the central and south-eastern zone of Peru, Near Cusco is Vilcanota/Urubamba River valley. located about 10 miles north of Cusco Peru, and extends northwest through Pisac and Ollantaytambo cities. Manned weather stations in Cusco. Just three automatic weather stations in this place.
  • 7. Rainfall Distributión Vilcanota River Basin Source: DCL/SENAMHI The rainfall incress between January 21-25 along the basin. High Basin Low Basin Medium Basin
  • 8. Historical Rainfall in January Pisac-Cusco The picture shows a high amount of rainfall in january, 2010
  • 9. Strong flow of Vilcanota river in Pisac, Cusco with 327 m3/s top exceed its historical values. Strong Flow of Vilcanota River of Cusco
  • 10. Source: Civil Defense Institute Rainfall Impacts in South Peru
  • 11. Source: Red Cross Flood Impacts in South Peru
  • 12. Flood Impacts in Cusco city
  • 13. Damage caused by floods in Cusco Source: EL COMERCIO Newspaper ( February 08, 2010) Deads 9 Injured people 10 Homes affected 10.325 Schools afected 35 Medical center affected 06 People affected 21.393 Losses 4 Homes destroyed 4.828 Schools destroyed 9 Medical center destroyed 02 Churchs affected 15 Public places affected 143 (losas, parques, estadios y otros) Losses (millions de US dolars) 250 Destroys railroads 6,15 km Affected railroads 2,45 km Asphalt roads destroyed 18 km Unpaved Road destroyed 11 km Track roads destroyed 56 km Track bridges destroyed 21 Track bridges affected 30 Fallen street light 477 Losen water intake 86 Farms destroyed (Ha) 16.281 Farms Affected (Ha) 10.950
  • 15. This figure shows the CLIMATE OUTLOOK issued to media, decision makers and stakholders before event Climate Forecast of Rainfall December 2009- February 2010 Extreme rainfall
  • 16. During January 2010 heavy rainfall affected south Peru, increase of river and floods in Cusco, especially in Pisac city. We observe incress activity of South Atlantic convergence zone that persisted for several days and brought unusually large levels of moisture to the South Peru. The good cooperation between SENAMHI, Civil Defense Institute and Economy Ministry, lead to finance one automatic weather station loosen during this unusual floods. At this moment there are a project supported by national government to deploy 12 automatic weather station in that place. This project was designed before this event. CONCLUSIONS
  • 17. To establish an Early Warning System is neccesary in Cusco region, to warning the population by natural disaster. To strengthen the capacity of local civil defense teams and organizations is necesary. To organize the population is requerid to improve the emergency management. Disaster Risk Management Specialists is necesary in order to manage the emergency and prevent future risks. RECOMMENDATIONS

Editor's Notes