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Current capabilities in the analysis of climate risks and adaptation strategies in critical

areas

M. Arif Goheer

Global Change Impact Studies Centre (GCISC) Islamabad- 44000, Pakistan

Symposium on Climate Change and Variability-Agro Meteorological Monitoring and Coping Strategies for Agriculture, Oscarsborg, Norway

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Climate Risk

Risk is generally considered to be a product of

consequences and likelihood - what can happen, and what are the odds of its happening

Uncertainty is a critical factor in assessing both climate risks and the effectiveness of different policy

strategies. Each climate risk is identified by its own natural characteristics, including geographical area, time of the year it is most likely to occur and its

severity.

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Types of climatic risks

1. Due to average changes in climate parameters*

2. Due to extreme events (floods, droughts, cyclones etc.)

*Temperature and precipitation as main climatic

variables of climate uncertainty

(4)

Tools for risk analysis

• Agro-climatic indices

• Statistical and econometric analysis

• Mathematical models

• community based participatory tools such as climate risk maps, community history, focus group meetings and historical transect, matrix rankings, seasonal

calendars and vulnerability indices etc.

(5)

Indices

• Climate indices are developed in a simplified way to communicate more complex climate change impact relations.

Mean temperature and precipitation sums can be seen as (simple) climate indices, other

examples may be Leaf area index, Potential

soil moisture deficit, Growing Degree Days etc.

(6)

Models

• Climate Models - GCMs

Provide data on climate variables

generally at a resolution of 300 x 300 Km

– Accurate Temperature prediction in most of the cases (IPCC report 25 models)

– Precipitation prediction still needs betterment

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- RCMs

Provides data on climate variables generally at a resolution of 30x30 by 50x50Km resolution.

A number of models available

Main ones are RegCM and PRECIS

Perform best in the areas where they are developed.

Large data set requirements for model evaluation

Generally the capability in most of the Asian countries is low in terms of seasonal (annual/interannual) prediction.

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• Hydrological models

– Used for water resources management studies

– A number of models available viz; VIC,HEC family of models, WASMOD, WEAP etc.

– Performance requires high input data which most of the countries do not have.

(9)

• Crop Models

– Can predict well the growing season length and yield for those areas where they have been established

– A long list of UNFCCC reported CSMs (DSSAT, APSIM, EPIC, WOFOST, etc.)

– Although for each region calibration is the prerequisite for the studies yet regional crop

coefficients needs to be changed in the models e.g;

base temperature requirements and light extinction coefficient.

(10)

– A comprehensive model which takes into account the varibales from sowing till economic analysis with a number of options for inputs, insect-pest

measurements, GHG emissions considerations is still awaited.

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Studies for extreme events

• Presently statistical analysis tools are employed for extreme event studies

• The prediction element is poorly reflected in these tools

• IPCC (2007) reports of more extreme events and natural disasters in the years to come.

• Urgent need to assess the forecasting skills of natural disasters to determine those where greater research is needed. Lack of good forecast skill in drought , for

example, is a constraint to improved management and adaptation.

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Impact of rise in temperature on wheat Growing Season Length in Northern and Southern parts of Pakistan

113 121

133 194

5

118 125

138 202

4

123 130

144 211

3

127 135

149 221

2

132 140

155 232

1

137 146

161 246

Baseline

Plains (Arid) Plains

(Semi-arid) Sub-Mountainous

Region (Sub-humid) Mountainous

Region (Humid)

Southern Pakistan Northern Pakistan

Growing Season Length (Days) Temperature

˚C

(increase over baseline)

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Wheat Yield in different agro- climatic zones of Pakistan under A2 Scenarios

2500 3000 3500 4000 4500 5000

Base 2020 2050 2080

Wheat Yield (kg/ha)

Northern Mountainous Region Northern Sub mountainous Southern Semi-arid Plains Southern Arid Plains

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Climate Change Impact on Wheat Production in Pakistan by 2085 under A2 and B2 Scenarios

-6 -5

4490 Southern Arid 47

Plains

- 6.4 - 5.7

4326 Pakistan 100

-8 -8

4306 42

Southern Semi arid Plains

-11 -11

3933 Northern Sub- 9

mountainous

+40 +50

2658 Northern 2

Mountainous

B2 Scenario A2

Scenario

% Change in yield in 2085 Baseline Yield

(kg ha-1)

% Share in National Production Region

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Effect of increase in Temperature on Growing Season Length of Rice in Semi arid areas of Punjab

(Cv. Basmati Super transplanted in 1st Week of July)

89 5

92 4

98 3

100 2

102 1

(increase over baseline)

108 Baseline

Growing Season Length (Days)

Temperature (°C)

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Basmati Rice Yield in Southern Semi-arid Plains of Pakistan under A2 and B2 Scenarios

3000 3200 3400 3600 3800 4000 4200 4400

1990 2025 2055 2085

Year

Rice yield (kg/ha)

Southern Semi -arid Plains A2 Southern Semi-arid Plains B2

Yield decrease by 2085:18% in A2 and 15% in B2 Scenarios

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Adaptation

• Refers to the responses and adjustments to climate change that may be used to reduce vulnerability and strengthen resilience

• It also relates to actions that exploit new

opportunities resulting from climate change

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Approaches

• Through policy and planning-Improving infrastructural base.

• Through actions or adjustment already being used to address climate change e.g., investment in drip

irrigation to address water scarcity.

• Addressing current problems to increase overall

resilience to climate change. e.g., economic reforms, improved management and increased monitoring.

• Technological and Engineering solutions- Costly but long term options. e.g., water desalination

(19)

Strategies

• Agronomic

– Change in Cropping Pattern/Cropping intensity – Changes in sowing and harvesting dates

– Choice of suitable varieties

– Appropriate cultural practices for warmer and drier climates e.g., deep tillage every 2-3 years to store rain water in soil profile

– Efficient Irrigation scheduling (based on critical growth stages and deficit amount)

– Weed management

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Strategies

(Contd…)

• Crop Breeding

Developing varieties from climate change perspective

• Short Duration

• High Temperature Tolerant

• Resistant to Abiotic (drought, salinity) and Biotic (insect pests and diseases) stresses

using conventional as well as mutation breeding and through biotechnology & genetic engineering

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Strategies

(Contd..)

Water conservation

Laser Land leveling

Shift in water management practices

Sprinkler irrigation Drip irrigation Pitcher irrigation

Bed and Furrow irrigation

Reduced tillage

Direct seeding

Subsurface irrigation channels in arid areas

Cycling /reuse of municipal, sewage and industrial effluents

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Emerging Sustainable

Farmers

Dynamic pathways: Linking present vulnerability to climate outlooks

Climate Forecasters

Dissemination Channels

Commercial Farmers

Vulnerable Farmers

Multi-agent approach:

•Represent actors as software agents

•Multi-level vulnerability

•Emergence from interactions

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Concluding Remarks

• Asia mostly arid , semi arid and rain-fed

• Accounts more towards farming to nourish its growing population

• Per capita land availability is low

• Most countries have the poor capacity to have sufficient knowledge of climate change to assess their impacts

and devise adaptation strategies respite some

developed/developing countries like Japan, Malaysia, China and India.

• Once the capability to assess the climate risks is there, the countries can perform cc impact studies more

rigorously and can better plan for adaptation strategies.

(24)

References

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