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Climate change and vulnerability of agricultural systems.
How do we handle with the challenges of future climate
impacts on agriculture? Case studies in Southern Italy
PhD Eugenia Monaco National Research Council – CNR- Ercolano- Italy
Beirut, the7th May 2015
Evaluation of crop adaptation to climate change in a hilly area of Southern
Italy cropped with durum wheat and grapevine
The adaptive response in rain-fed condition was determined in two climate cases:
the reference (1961-1990) and the future (2021-2050) for two species
Objective
The intra-specific biodiversity was taken in account as a strategy
to cope with climate change
Durum wheat Grapewine
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Six Global Climate Models AOGCM (A1b) ( Ensembles
runs)
Daily Tmin Tmax TnTTmax, rain
Seasonal Tmin Tmax
rain
Weather generator
Statistical Downscaling
LOCAL AND REGIONAL OBSERVATION ERA40/CRA-CMA
Daily meteorological data applied in the simulation runs refer to two time periods,
namely “reference” (1961-1990 years) and “future” (2021-2050 years), the latter
constructed by applying statistical downscaling to GCMs scenarios.
1. Climate scenarios
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2. Agro-hydrological model
From output was calculated Crop Water Stress Index CWSI:
CWSI = 1 - ETact
ETpot
SWAP is a physically based model that calculate water flow through the Richards’
equation
Crop parameters derived from literature and taking in account the traditional
cropping system of study area
Mo
del in
pu
t
Soil Unit
Climate Reference
Future
Crop Species
parameters
Output
ETact
Tact
Soil water regime
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Hydrologic indicator
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3 . Temperature indicators
• Cultivar specific
Amerine and Winkler index
The thermal index of Amerine and Winkler (A&W,
1944) is the thermal sum of average daily
temperature (Tm)minus the zero vegetative of vine
plant (10°C) in the period between 1 April and 31
October.
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4. Hydrological requirements yield response function for food crops
(corn, wheath, barley, .soybean..)
y = -1.045x + 1.0294R² = 0.922
0
0.1
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0.3
0.4
0.5
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0.8
0.9
1
0 0.1 0.2 0.3 0.4 0.5 0.6
Yr
CWSI
• Cultivar specific
• Durum wheat is caraterized by a linear relation function
• A relative yield of 90% was consider as accetable
CWSI
cv
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5. Evaluation of cultivars’ adaptability ( crop production and/or quality):
temperature e regimi idrici….
CWSI simulated
Hydrologic indicator
CWSI cv specific and standard error
Hydrologic requirement
Probability of adaptation for each cultivar, soil and year
Medians were then used to assess and quantify the adaptability of cultivars in the
reference and future climate
Matching
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Case study: Durum wheat
Study area: Fortore, Benevento
Vineyards
Olives
Cereals
•The study area is a hilly area of the province of Benevento called "Fortore Beneventano”
• The area is of approximately 40,000 ha.
Case study: Durum wheat
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Study area: Fortore,
Benevento
Hills of clay marl and sandstone of Fortore
Hills of clay marl and sandstone of Miscano-Ufita
Hills of clay marl and sandstone of Tammaro
Three main landscape system
The Fortore geomorphology is mainly characterized by clayey and marl flysch hills and
highlands; narrow alluvial planes and small sandstone relieves are also included.
Case study: Durum wheat
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Durum wheat
The three soil profiles are associated to the main landscape systems.
Vertic- Inceptisol Vertisol Inceptisol
The soils of study area:
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Measured hydraulic properties (Wind’s method)
Durum wheat
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Results
1. Climate
Min, max temperatures and rain with standard deviation in the
Fortore area, for the cropping season of durum wheat
Climate Scenario Tmin (°C) Tmax (°C) Rain (mm)
1961-1990 5.5 (±4.05) 13.5 (±5.35) 563 (±50)
2021-2050 6.7 (±4.24) 15.2 (±5.76) 475 (±48)
Difference [(2021-50)- (1961-90)] 1.2 1.7 -88
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0
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
0.45
0.5C
WSI
Year
Vertisol
Vertic inceptisol
Inceptisol
2. SIMULATION OUTPUT- CWSI
• CWSI is a soil-dependent index
• High inter soil annual variability
• The values of CWSI in Vertisol ranging between 0.09 and 0.45.
• Vertic Inceptisol shows a range between 0.05 and 0.28
• Inceptisol ranging between 0.02 and 0.35
Results
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3. CULTIVARS’ REQUIREMENTS
• Durum wheat cultivars cropped in Mediterranean Country
• CWSI cv range between 0,05 and 0,21
Results
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3. CULTIVARS’ ADAPTATION
0%10%20%30%40%50%60%70%80%90%
100%
61-90 21-50
Waha 58% 19%
Haurani 74% 52%
Bacali 85 0% 0%
Cham 5 8% 1%
Cham 1 0% 0%
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apta
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n p
rob
abili
ty %
Vertisol
• The cultivar most adaptable is Haurani (p = 74% 61-90, p= 52% 21-50)
• The other cultivars ranging from 58 to 0% (0= not adaptable)
• The high difference in the two climates scenario is due to the lower rainfall and to the soil hydraulic
properties (low hydraulic conductivity that generates anoxic conditions during and after a rainfall event)
Results
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3. CULTIVARS’ ADAPTATION
0%10%20%30%40%50%60%70%80%90%
100%
61-90 21-50
Waha 100% 98%
Haurani 96% 94%
Bacali 85 76% 61%
Cham 5 80% 69%
Cham 1 0% 0%
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apta
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n p
rob
abili
ty %
Vertic Inceptisol
• The best cultivar is Waha, with the 100% of adaptation in the 61-90 and 98% in 21-50
• The other cultivars have a probability of adaptation ranging from 96 to 0%
• This soil is the best one in terms of durum wheat adaptation responses in both climate cases
•This soil has high water retention that allow a good soil water management during the wheat
cropping season
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3. CULTIVARS’ ADAPTATION
0%10%20%30%40%50%60%70%80%90%
100%
61-90 21-50
Waha 100% 90%
Haurani 96% 88%
Bacali 85 82% 16%
Cham 5 84% 38%
Cham 1 0% 0%
Ad
apta
tio
n p
rob
abili
ty %
Inceptisol
• The best cultivar is Waha, with a 100% adaptation probability in the 61-90 and 90% in the 21-50
• The other ones range from 96 to 0% in both climate scenarios.
• This soil could be considered suitable to durum wheat cultivation as well as the vertic inceptisolsoil
Results
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Conclusions case study 1
In the study area of Southern Italy “Fortore” the water regime of soils was predicted
by means of a hydrological model, coupled with future climate scenarios
• According to indicators and requirements, the adaptability of five cultivars of durum
wheat was different between the two climate periods.
• Results are strongly influenced by the rainfall distribution and by soils’ physical
properties, which determine soil water balance and then the crop yield responses.
• The intra-specific biodiversity of agricultural crops is a powerful tool for adaptation.
However soils’ water regime and yield responses have to be quantitatively assessed
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Case study: grapewine
It is a complex geomorphological area of 20,000 ha in Campania Region vocated to the
production of high quality wine (DOC and DOCG).
Study area: Valle Telesina
Landscape and soils information
The landscape has a complex
geomorphology and it is characterized by
an E-W elongated graben where the
Calore river flows. The area shows five
different geomorphic environments.
The parent material is very heterogeneous
especially in hills and terraces, which
determines an high soil spatial variability
(e.g. Calciustepts, Ustorthents, Haplustolls,
Hapludands and Haplustepts).
Soil information were derived from a soil
map at 1:50,000 scale (Terribile et al.,
1996) consisting of 47 soil mapping units
and soil typological units.
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Results
Thermal regimes evaluation... The climate and the water stress affect the vine growth and determine the character of the wine (Saayman, 1977,Matthews and Anderson, 1988;Van Leeuwen et al. 2004).
(DD
A)
Amerine & Winkler index values (DDA, degree day) in the reference and future climate
conditions. (in the figure the value of climatic period 2000-2009 is also reported)
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Amerine & Winkler index distributions in the reference and future climate, compared
with the specific thermal need of four cultivar (Falanghina, Aglianico, Malvasia,
Guarnaccia).
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Results
Soil moisture regimes evaluation... The physically based model SWAP was run in the "reference" and "future" climatic
period for all 47 soil units of study area. The Crop Water Stress Index (CWSI), was
calculated daily over the growing season in each climatic period.
0
50
100
150
200
250
300
350
400
450
Shoot growth Flowering Berry formation Berry ripening
mm
Rain cum. Reference
Rain cum. Future
The figure shows the average value over the two climate periods (reference and
future) of the rainfall cumulated in the four different vine development stages (shoot
growth, flowering, berry formation and berry ripening)
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Results
CWSI average over the whole season 198 days
Reference climate (1961-1990) Future climate (2021-50)
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Results
Reference climate (1961-1990) Future climate (2021-50)
No difference in this phenological phase
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Results
Reference climate (1961-1990) Future climate (2021-50)
Few differences in this phenological phase
In this phenological phase higher values of CWSI
may reduce the yield of grape and the quality of
wine
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Results
Reference climate (1961-1990) Future climate (2021-50)
Few differences in this phenological phase
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Results
Reference climate (1961-1990) Future climate (2021-50)
Many differences in this phenological phase
In this phenological phase an higher value of
CWSI may increase the quality of wine
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Conclusions case study 2
• An increase of Amerine & Winkler index is foreseen in the future climate
conditions (Fig.1); the increase reduces the adaptability of some important
cultivars (e.g. Aglianico and Falanghina) and improves the adaptability of some
others (e.g. Guarnaccia which is less important).
• In the future climate scenario, the CWSI, cumulated over the growing season,
has shown an average increase of 5-8 % , with marked increase in the berry
formation and berry ripening phenological phases.
• In some area (e.g. the ancient terraces) the soil characteristics have mitigated the
effects of climate change showing the same behaviour of CWSI in both climate
scenarios.
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References
Climate change, effective water use for irrigation and adaptability of maize:
a case study in Southern Italy. Monaco E., Bonfante A., Silvia Maria Alfieri,
Angelo Basile, Massimo Menenti and Francesca De Lorenzi. Biosystem
Engineering, 128 pp 82-99 (2014).
http://dx.doi.org/10.1016/j.biosystemseng.2014.09.001
Adaptation of irrigated and rainfed agriculture to climate change: the
vulnerability of production systems and the potential of intra-specific
biodiversity. Case studies in Italy. Menenti M, Alfieri SM, Bonfante A, Riccardi
M, Basile A, Monaco E, De Michele C, De Lorenzi F, 2014. Handbook of Climate
Change Adaptation. DOI 10.1007/978-3 642-40455-9_54-1.
Editore/ISBN/ISSN/EAN Springer-Verlag Berlin Heidelberg.
http://link.springer.com/referenceworkentry/10.1007/978-3-642-40455-9_54-1
Climate change effects on the suitability of an agricultural area to maize
cultivation: application of a new Hybrid Land Evaluation System.
Bonfante, A., E. Monaco, S.M. Alfieri, F. De Lorenzi, P. Manna, A. Basile,
and J. Bouma. 2015. Advances in Agronomy (in press).
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