Agriculture Reference
In-Depth Information
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Table 12.2 Climatic classification and aridity index based on
methodology by Thornthwaite and Mather (1955) for distinctive
locations in Argentina, Brazil, Chile, and Paraguay
Country
Location
Aridity index
Climate
Argentina
Rivadavia
0.48
Semiarid
Mendoza
0.75
Arid
Chepes
0.66
Arid
Brazil
Quixeramobim (NE)
0.48
Semiarid
Petrolina (NE)
0.75
Arid
Jaguaribe (NE)
0.58
Semiarid
Fortaleza (NE)
0.33
Subhumid, humid
Cuiab a (W)
0.13
Subhumid dry
Ribeir ao Preto (SE)
0.09
Humid
Barretos (SE)
0.13
Subhumid, humid
[161
Campinas (SE)
0.03
Humid
Chile
Los Andes
0.63
Semiarid
Patrerilios
0.89
Arid
La Serena
0.79
Arid
Line
——
0.1
——
Norm
PgEn
Antofogasta
0.99
Arid
Paraguay
Pedro Pe na
0.54
Semiarid
Nueva
0.54
Semiarid
Mariscal
0.45
Semiarid
D istribution of Dry Spells
The occurrence of dry spells lasting more than 10 days in the month of
January seriously affects the production of field and grain crops, partic-
ularly field and grain crops in the southeastern and central parts of the
country (Alfonsi et al., 1979), and the knowledge of the distribution of the
dry spells is helpful in identifying, quantifying, and mapping droughts in
the region (Arruda and Pinto, 1980).
Drought monitoring and mitigation in Brazil is in its initial stage. Only
the state of S ao Paulo conducts weekly drought monitoring—through its
Integrated Agrometeorological Information Center (CIIAGRO) and the
Instituto Agronômico de Campinas (IAC-APTA) of the Agriculture and
Supply Secretariat (Government of the State of S ao Paulo)—using various
indices (Brunini et al., 1998) that are described below.
[161
So il Moisture and Potential Evapotranspiration
The ratio of the actual water availability in soil (W) to the maximum
water availability in soil (Wx) and PET can be used to monitor drought
conditions, as shown in table 12.3.
Currently a new index, the agricultural drought index (ADI), as shown
in table 12.4, is being implemented to monitor crop development stages
and drought conditions. The ADI takes into account not only the actual
soil water availability, but also the crop phenological stages and rainfall
distribution.
 
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