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Curso de Climatología Sinóptica en la Costa Oeste de América del Sur Abril 2007; Lima - Perú

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SENAMHI – Perú

Curso de Climatología Sinóptica en la Costa Oeste de América del Sur

16-20 Abril 2007; Lima - Perú

Relator: Dr. René D. Garreaud

www.dgf.uchile.cl/rene

Departamento de Geofísica

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Presentación No. 1: Climatología de Sud América

En esta exposición se describe el clima actual de Sud América empleando observaciones

instrumentales durante el siglo XX. La exposición comienza con una descripción de las bases

de datos disponibles para efectuar tal climatología. Luego, se provee un entendimiento básico

de los procesos físicos que explican la distribución promedio y el ciclo anual medio de las

variables meteorológicas (precipitación, temperatura, vientos) sobre el continente Sud

Americano y los océanos adyacentes. También se describen en forma sucinta los patrones

continentales de variabilidad climática asociados con ENSO, PDO y AAO.

Fuentes de datos para estudios de climatología

Circulación global y contexto geografico

Patrones de circulación continental

Variabilidad interanual

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Surface and Upper

Air Observations

Satellite Products

Assimilation

system

Gridded Analysis

Gridding

method

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Table 1. Main features of datasets commonly used in climate studies

Dataset Key references Input data -Variables Spatial resolution -Coverage Time span -Time resolution Station GHCN

Peterson and Vose (1997)

Sfc. Obs Precip and SAT

N/A Land only

1850(*) – present Daily and Monthly

Gridded GHCN

Peterson and Vose (1997)

Sfc. Obs Precip and SAT

5° 5° lat-lon Land only

1900 – present Monthly

Gridded

UEA-CRU New et al. 2000

Sfc. Obs Precip and SAT

3.75° 2.5° lat-lon Land only 1900 – present Monthly Gridded UEA-CRU05

Mitchell and Jones (2005)

Sfc. Obs Precip and SAT

0.5° 0.5° lat-lon Land only 1901 – present Monthly Griddded U. Delware

Legates and Willmott (1999a,b)

Sfc. Obs Precip and SAT

0.5° 0.5° lat-lon Land only 1950 – 1999 Monthly Gridded SAM-CDC data

Liebmann and Allured (2005) Sfc. Obs Precip 1° 1° lat-lon South America 1940 – 2006 Daily and Monthly

Gridded

CMAP Xie and Arkin (1987)

Sfc. Obs.; Sat. data Precip

2.5° 2.5° lat-lon Global

1979 – present Pentad and Monthly

Gridded

GCPC Adler et al. (2003)

Sfc. Obs.; Sat. data Precip 2.5° 2.5° lat-lon Global 1979 – present Monthly NCEP-NCAR Reanalysis (NNR) Kalnay et al. 1996 Kistler et al. 2001

Sfc. Obs.; UA Obs; Sat. data Pressure, temp., winds, etc.

2.5° 2.5° lat-lon, 17 vertical levels Global 1948 – present 6 hr, daily, monthly ECMWF Reanalysis

(ERA-40) Uppala et al. (2005)

Sfc. Obs., UA Obs, Sat. data Pressure, temp., winds, etc.

2.5° 2.5° lat-lon, 17 vertical levels Global

1948 – present 6 hr, daily, monthly

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Surface (land/ocean) Synoptic Stations

Met. Observations (T,Td,P,V,…) @ 0, 6, 12, 18 UTC are

transmitted in real-time to WMO and Analysis Centers

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Red de Radiosondas (OMM, GTS)

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Observaciones en altura IV:

Info. Obtenida por Aviones comerciales

Perfiles verticales (0-10 km) de T, HR, viento, presión, y datos a

nivel (10 km) a distintas horas. También se transmiten via GTS

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All stations (anytime, any length)

Century-long stations (Ti<1905, Tf>1995, missdata<20%)

Precipitation

Mean Temperature

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Because analysis are produced in real-time, some data

is not assimilated, but it was archived. In the 90’s the

NCEP-NCAR (USA) began a major project in which

they re-run their assimilation system with all the

available data.

The result is the widely used “Reanalysis” data,

including many fields (air temperature, wind, pressure)

on a regular

2.5°x2.5° lat-lon grid

, from

1948 to present

every 6 hours (also available daily, monthly and long-

term-mean means). Fields are 2- or 3-Dimensional.

Preferred data format: NetCDF.

Freely available.

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Reanalysis system also includes a meteorological

model from which precipitation and other not-observed

variables (e.g., vertical motion) are derived.

Reanalysis data is great for studying interannual and

higher frequency variability.

Interdecadal variability and

trends are not so well depicted (we don’t trust much

before the 70’s, particularly in the SH).

European Center (ECMWF) did a similar effort (ERA-

15 and ERA-40). Higher horizontal resolution

(1.25°x1.25°), but harder to get.

Reanalysis

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Jan

Jun

Climatology of 300 hPa winds

(10-12 km) from NNR

Example of some daily fields

from NNR

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Altiplano

Subtropical

Andes

Amazon basin

La Plata

basin

Brazilian

highlands

Chaco

Pampas

Patagonia

Equatorial

Andes

Llanos

Guinas

highlands

Geographical

setting

10°N

0°N

20°S

40°S

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Because of its long meridional extent, South America

exhibits tropical, subtropical and extratropical climatic

regimes

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(15)

15

1

2

3

4

5

6

7

8

1

9

10

5

6

1

2

3

4

1

2

3

4

Precipitation features

1. ITCZ

2. Continental convection

3. Altiplano convection

4. SACZ

5. Pampas convection

6. Midlatitude storm track

7. Orographic precipitation

8. Coastal desert

9. NE Brazil semiarid

10. Patagonia dry zone

11. Ocean desert

Circulation features

1. ITCZ

2. Trade winds

3. Subtropical high

4. Midlatitude westerlies

5. Low level jet

6. SACZ

7. Bolivian high

8. NE Brazil trough

9. Tropical easterlies

10. Midlatitude westerlies

11. Jet stream

7

8

9

10

11

11

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Annual Mean / Zonal Mean

Annual Mean / Zonal asymmetry

January - July Mean

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17

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Modest annual cycle in the extratropics

4

1

2

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(20)

The Precipitation Variability (UdW data)

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Stronger than normal westerlies leads to rainy conditions over western Patagonia

BUT drier conditions over eastern Patagonia (orographic effects)…not much

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Annual mean Precip/SAT regressed upon

index of large-scale modes (50 years of data)

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Seasonal correlation between Precip/SAT and

Multivariate ENSO Index (50 years of data)

Referencias

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