Transcript of El Niño-Southern Oscillation (ENSO) cycle events and their ...
El Niño-Southern Oscillation (ENSO) cycle events and their impacts
in Zimbabwe
Zimbabwe Resilience Building Fund
El Niño-Southern Oscillation (ENSO) cycle events and their impacts
in Zimbabwe
December 2016
© UNDP 2017
This publication may be reproduced in whole or in part and in any
format for educational, research and/or non-profit purposes without
special permission from the copyright holder, provided
acknowledgement of the source is made. Analysis and write-up are
credited to staff from the following organisations, ZRBF, AGRITEX,
Meteorological Services Department, Livestock Production Division
and the Zimbabwe National Water Authority (ZINWA).
These are: Vhusomuzi Sithole, Rufael Fassil, Natalia Perez,
Takudzwa Mutize, Hillary Mujiyo, Robson Chihumba,Vimbai Mamombe,
Blessing Shumba, Nyashadzashe Viriri and Debra Musiwa.
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For bibliographic and reference purposes, this publication should
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“UNDP (2017), El Niño-Southern Oscillation (ENSO) cycle events and
their impacts in Zimbabwe”.
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UNDP Zimbabwe, Zimbabwe Resilience Building Fund (ZRBF) Management
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Harare, Zimbabwe +263 4 338836-44
Contents 1. EXECUTIVE SUMMARY 5
2. INTRODUCTION 6
3. METHODOLOGY 9
3.1 Data Analysis 9
3.2 Scenario building to inform climate change and resilience
building projects in
Zimbabwe 12
4.3 Impacts on maize production 14
4.4 Impacts on cattle production 17
4.5 Impacts on water resources 19
4.6 Scenario planning 21
Annex 2: Dam levels by catchment area 28
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List of Figures Figure 1: Zimbabwe Standardized Precipitation Index
(SPI) and Sea Surface
Temperature (SST) anomalies 11
Figure 2: National maize production statistics since 1980 12
Figure 3: Maize yield map for the 2015/16 agricultural season.
12
Figure 4: Maize yield map for the 2014/15 agricultural season.
13
Figure 5: Provincial maize yield for the different ENSO classes
13
Figure 6: Friedman’s test results for different EBSO classes
14
Figure 7: Cattle Populations for the period 2000-2016 14
Figure 8: Friedman’s test results on cattle population across
different ENSO classes 15
Figure 9: Percentage Inflow for all major dams (1972-2016) 15
Figure 10: Dam level figures per catchment across different ENSO
classes 16
Figure 11: Friedman’s test results for dam levels in different
catchments 16
List of Tables Table 1: Proposed data sources 8
Table 2: Classification of ENSO events for the period 1951-2016
10
Table 3: Categories of rainfall received under different ENSO
events 11
Table 4: Summary of impacts under different La Niña scenarios
17
Table 5: Summary of implications to climate change and resilience
programmes in
Zimbabwe 17
1. EXECUTIVE SUMMARY The 2015/16 rainfall season resulted in
Zimbabwe experiencing low and erratic rains mainly due to El Niño
conditions. The Seasonal Outlook for the 2016/17 season predicted
normal to above normal rainfall due to La Niña/Neutral conditions
in the Pacific Ocean. This technical note evaluate impacts of the
different phases of the El Niño-Southern Oscillation (ENSO) cycle
on dam levels, maize and cattle production. The impacts were
evaluated through trends analysis and overlaying ENSO events and
each of the three variables (dam levels, maize and cattle
production). The objectives of the technical note are to document
the impacts of the 3 phases of ENSO (El Niño, Neutral and La Niña)
in Zimbabwe and develop planning scenarios. These scenarios examine
the possible dam levels, maize and cattle production in a season
when La Niña/Neutral conditions are predicted. Potential
consequences on resilience programme activities were also
documented in these scenarios.
Results show that the 62% of El Niño events have led to below
normal rainfall in Zimbabwe since 1970. In turn, the low rainfall
has negatively affected dam levels, maize and cattle production in
the country. On the other hand 67% of La Niña events over the same
time period have resulted in above normal rains. The improved rain
resulted in higher dam levels, maize and livestock production when
compared to El Niño years. It is important to note that some of the
La Niña events have resulted in flooding in some parts of the
country thereby negatively affecting maize and cattle production.
The last phase of ENSO, saw the country receiving above normal
rainfall 54% of these Neutral years. Dam levels were average
compared to El Niño and La Niña. However, neutral years have
resulted in the highest yields due to optimum rains. Statistical
analysis proved that dam levels, maize as well as cattle
populations significantly differ when compared across different
ENSO classes. When the rainfall, dam level, maize and cattle
production analysis was related to resilience programming
activities and the national seasonal climate forecast for 2016,
there is evidence that most of the activities will be disrupted if
the country experiences medium or strong La Niña. However, if a
weak La Niña or Neutral phenomenon occur, information from previous
years show less chances of disruption with maize and cattle
population expected to be higher compared to strong La Niña or El
Niño years.
In a nutshell, this technical note shows that that ENSO events
significantly impacted the production systems in the country. It is
therefore recommended for resilience building initiatives to plan
according to predicted phases of ENSO.
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The 2015-2016 drought experienced across Zimbabwe has been
attributed to the El Niño phenomenon. The most affected regions
include the western, southern and south- eastern districts of
Zimbabwe. Zimbabwe experienced similar drought conditions in 1982,
1992 and 2012. El Niño and La Niña are opposite phases of the El
Niño-Southern Oscillation (ENSO)1 cycle. The “El Niño” phenomenon
refers to the large-scale ocean- atmosphere climate interaction due
to warming of sea surface temperatures across the central and
east-central Equatorial Pacific Ocean, which results in drought
conditions for Southern Africa2. Meteorological drought results
from prolonged periods of below average rainfall for a season or
more3. In Zimbabwe, the El Niño phenomenon often leads to drought
conditions with negative effects on livelihoods. On the other hand,
the La Niña phenomenon is characterised by anomalously cool sea
surface temperatures in the Pacific Ocean thereby affecting global
climate in an opposite way to El Niño. In the case of Zimbabwe,
often leading to increased rainfall conditions.
In Zimbabwe, legal and institutional frameworks for disaster risk
management are well established at both local and national levels.
Disaster management is multi-sectoral and involves various relevant
ministries and institutions, coordinated by the Department of Civil
Protection (DCP) within the context of the National Civil
Protection Committee (NCPC). The institutions include government
ministries, parastatals, private sector, United Nations agencies,
and non-governmental organisations. These various institutions
provide different capacities for DRM in the country.
A number of policies and legislation guide the operations of DRM at
various scales in the country. The Hyogo Framework for Disaster
Risk Reduction and Management was the widely used policy framework
in developing the various national statutes. The National statutes
include the Civil Protection Act No. 5 of 1989, National Climate
Change Strategy for Zimbabwe, National Water Policy, Meteorological
Services Act and Zimbabwe Food Security Strategy. The DCP is guided
by the Civil Protection Act which provides for the establishment of
the Department of Civil Protection and setting up of the
1. NOAA (2016), What is La Niña?
http://www.pmel.noaa.gov/elnino/what-is-la-nina. 2. NOAA (2016),
What are El Niño and La Niña? http://oceanservice.noaa.gov/facts/
ninonina.html 3. Chitongo (2013), Towards Comprehensive Disaster
Risk Management in Zimbabwe: Evaluating Masvingo Rural District’s
Community Drought Management Program (MRDCCDMP), International
Journal of Economy, Management and Social Sciences, 2(8).
National Disaster Management Committee. In addition, international
organisations such as UNDP and UNOCHA are also guided by the
provisions of the HYOGO framework for Disaster Risk Reduction and
Management (2005-2015), the Sendai Framework for Disaster Reduction
(2015-2030), the United Nations Framework Convention on Climate
Change (UNFCC) and the Paris Agreement on Climate Change which
entered into force on 4 November 2016. This technical note also
supports the national efforts in meeting the SDGs especially Goals
number 2 (Zero Hunger), 3 (Good Health and well-being), 10 (Reduced
Inequality) and 13 (Climate Action). The technical note will
further more contribute to Outcome 1 (Food and Nutrition Security)
of the Zimbabwe United Nations Development Assistance Framework
(ZUNDAF) 2016-2020.
The Government of Zimbabwe is partnering UNDP in areas related to
climate change, resilience and poverty reduction. Most of these
initiatives, particularly the climate change and resilience
programmes, seek to assist the government in fostering
preparedness, early warning, early action and resilience building
activities in the face of disasters. Since the government’s
declaration of the 2015-2016 drought as a State of Disaster, UN
Agencies and civil society organisations are rendering humanitarian
assistance in a number of affected districts. This is a costly
exercise, which diverts funds from productive investment and which
has proven to have a negative impact on the beneficiary population
in the form of dependency syndrome. In order to minimise the impact
of similar situations in the future it is essential for all
mandated government departments to work together in developing a
long term strategy for mitigating impacts of both El Niño and La
Niña. There are a number of questions concerning the El Niño and La
Niña impacts which this technical note attempts to answer based on
analysis of data collected by four national departments in
collaboration with the Zimbabwe Resilience Building Fund (ZRBF).
These include Agricultural Extension Services Department (AGRITEX),
Division of Livestock Production and Development, Meteorological
Services Department (MSD), Zimbabwe National Water Authority
(ZINWA), and the Department of Civil Protection (DCP).
2.1 Justification and Objectives
In 2016, Zimbabwe, like the rest of the Southern African region,
was experiencing the consequence of the worst drought in 35 years.
The 2015-2016 drought resulted in loss of both domestic4 and wild
animals, crop failure as well as lack of adequate water
availability for both domestic use and industrial use. This has
culminated in low yields and food insecurity in many parts of the
country. The subsequent 2016 ZimVAC estimated that about 4.1
million people will need food assistance during the peak of the
season (January
4. El Niño and drought take a toll on Zimbabwe’s cattle, Thomson
Reuters Foundation News, Tuesday 12 January 2016,
http://news.trust.org/item/20160112054900-bk2q7/?-
source=spotlight.
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to March 2017)5. Figures from the Livestock Production and
Development Division show that there were more than 25 000 cattle
deaths which are attributed to the El Niño induced drought
countrywide. The government declared the drought conditions a State
of Disaster on the 4th of February 2016.
The frequency of unreliable weather patterns (e.g. false and late
starts of agricultural season combined with long of mid-season dry
spells) as well as anticipation of El Niño and La Niña conditions
create the need for accurate and reliable information. Information
generation and dissemination will foster learning from past
experiences as well as creating early warning systems resulting in
early action on forecasted events. This technical note seeks to
contribute some of the information on the consequences of the three
phases of ENSO, namely El Niño, La Niña and Neutral.
Specific Objectives
The specific objectives of this technical note are to:
• Document the causes, historical trends and effects of the El Niño
phenomenon in Zimbabwe,
• Document the causes, historical trends and effects of the La Niña
phenomenon in Zimbabwe, and
• Develop scenarios on for the La Niña phenomenon and Neutral
phases, as predicted in the latest weather outlook.
5. Zimbabwe Vulnerability Assessment Committee (ZimVAC) 2016 Rural
Livelihoods Assessment.
3. METHODOLOGY The analysis of ENSO impacts was carried out at a
national level, based on existing quantitative data obtained from
the mandated government departments. Government reports, bulletins
and official communication were used as complementary qualitative
data sources. Quantitative data on drought and El Niño frequency
were obtained from the meteorological datasets. The following table
summarises the various data sources.
Table 1: Proposed data sources
Variable Data source Period of time
El Niño /La Niña frequency and impacts MSD 1951-present
El Niño and La Niña’s impacts on rainfall MSD 1971-present
El Niño /La Niña effects on crops AGRITEX 1980-present
El Niño /La Niña effects on livestock LPD 1980-present
El Niño /La Niña effects on dam levels ZINWA 1972-present
Scenario building to inform climate change and resilience building
projects in Zimbabwe
UNDP
3.1 Data Analysis The methods used in data analysis were determined
by the type of data obtained namely meteorological, crops
production, livestock production and water resources. Each method
is described in detail in the below.
ENSO Trends Analysis Sea surface temperatures anomalies in the
Pacific Ring were analysed and subsequently seasons were classified
into Weak, Moderate, Strong, Very Strong, El Niño events. Sea
surface temperature is the temperature of the top millimetre of the
ocean’s surface. An anomaly is a departure from average conditions.
Sea surface temperatures anomaly maps compare temperatures in a
given month to the long- term average temperature of that month. At
irregular intervals (roughly every 3-6 years), the sea surface
temperatures in the Pacific Ocean along the equator become warmer
or cooler than normal. These anomalies are the hallmark of El Niño
and La Niña climate cycles, which can influence weather patterns
across the globe. On the other hand, strong, localized sea surface
temperature anomalies may reveal that an ocean current has veered
off its usual path for a time or is stronger or weaker than usual.
Sea surface temperature anomalies that persist over many years can
be signals of regional or global climate change, such as global
warming.
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Meteorological Data Analysis RRainfall data for the years 1981 to
2016 were merged with information on occurrence of El Niño, Neutral
and La Niña events, to determine the impacts on Zimbabwe’s
rainfall. In consultation with other specialists, total rainfall
for the months which are critical for crop growth was plotted
against time. The meteorological data were used to classify
rainfall seasons from 1981 to present into different ENSO
classes.
The Standardized Precipitation Index (SPI) is a tool which was
developed primarily for defining and monitoring drought. It allows
an analyst to determine the rarity of a drought at a given time
scale (temporal resolution) of interest for any rainfall station
with historic data (McKee et al 1993; McKee et al 1995; Guttman,
1998; Guttman, 1999; Trenberth et al., 2014). It can also be used
to determine periods of anomalously wet events. The SPI is not a
drought prediction tool. Mathematically, the SPI is based on the
cumulative probability of a given rainfall event occurring at a
station. The historic rainfall data of the station is fitted to a
gamma distribution, as the gamma distribution has been found to fit
the precipitation distribution quite well. This is done through a
process of maximum likelihood estimation of the gamma distribution
parameters, α and β. In simple terms, the process described above
allows the rainfall distribution at the station to be effectively
represented by a mathematical cumulative probability function.
Therefore, based on the historic rainfall data, an analyst can then
tell what is the probability of the rainfall being less than or
equal to a certain amount. Thus, the probability of rainfall being
less than or equal to the average rainfall for that area will be
about 0.5, while the probability of rainfall being less than or
equal to an amount much smaller than the average will be also be
lower (0.2, 0.1, 0.01 etc., depending on the amount). Therefore if
a particular rainfall event gives a low probability on the
cumulative probability function, then this is indicative of a
likely drought event. Alternatively, a rainfall event which gives a
high probability on the cumulative probability function is an
anomalously wet event. Negative SPI values represent rainfall
deficit, whereas positive SPI values indicate rainfall surplus.
Intensity of drought event can be classified according to the
magnitude of negative SPI values such that the larger the negative
SPI values are, the more serious the event would be. For example,
negative SPI values greater than 2 are often classified as
extremely dry conditions. An advantage in using SPI is that only
rainfall data are needed for its computation. SPI can also be
compared across regions of different climatic zones. The SPI index
for Zimbabwe for the period 1960 to date, was calculated from
rainfall data collected from 44 stations across the country.
Crop and Livestock Production Data Analysis Using data from the
crop and livestock surveys, national, provincial and district level
maps and trends were plotted. Using maize production data from
different ENSO classified years, analysis was done to check if
there was any significant difference in
production levels between the years affected by El Niño events vs
“normal” years. The non-parametric, Friedman’s test was used to
detect differences in production levels across multiple years. The
Friedman’s test was selected since the data was found not to be
normally distributed.
The null hypothesis for the Friedman’s test was:
Ho: μ1 = μ2 = μ3 Means of production data (crop/livestock) are not
significantly different across the different years
H1: μ1 ≠ μ2 ≠ μ3 Means of production data (crop/livestock) are
significantly different across the different years
Water Resources Data Analysis Dam levels data were analysed for
trends in water levels, as well as occurrence of flooding events
over the period 1972 to 2016. Similarly, an analysis of the
significant difference among ENSO years using the Friedman’s test
was conducted to test if there were any significant difference in
inflows across the years.
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3.2 Scenario building to inform climate change and resilience
building projects in Zimbabwe Based on these analyses, the next
stage involved developing scenarios of how the La Niña and Neutral
phenomenon will affect agricultural production (crops and
livestock) as well as water resources in the coming seasons.
Different classes of La Niña were used to build the scenarios.
Conclusions were made on the El Niño/ La Niña impacts on water
resources, crop and livestock production in Zimbabwe. These fed
into the evaluation on the implications of the different scenarios
to climate and resilience building programmes in Zimbabwe. The
information generated in this exercise is complementary to the
2016/2017 seasonal outlook since it evaluates past experiences as a
way of providing information on anticipated impacts.
4. RESULTS Results on ENSO Trends as well as impacts on rainfall,
dam levels, maize and cattle production in Zimbabwe are presented
as follows:
4.1 ENSO Trends
An analysis of the sea surface temperatures anomalies in the
pacific ring produced the following classification of
seasons.
Table 2: Classification of ENSO events for the period
1951-2016
El Niño La Niña Neutral Weak Mod Strong Very
Strong Weak Mod Strong Neutral
1951-52 1963-64 1957-58 1982-83 1950-51 1955-56 1973-74
1960-61
1952-53 1986-87 1965-66 1997-98 1954-55 1970-71 1975-76
1962-63
1953-54 1987-88 1972-73 2015-16 1964-65 1998-99 1988-89
1966-67
1958-59 1991-92 1967-68 1999-00 1978-79
1968-69 2002-03 1971-72 2007-08 1980-81
1969-70 2009-10 1974-75 2010-11 1985-86
1976-77 1983-84 1989-90
1977-78 1984-85 1993-93
1979-80 1995-96 2008-09
1994-95 2000-01 2001-02
2004-05 2011-12 2003-04
The most notable information coming out the classification is
that:
• The 2015/16 season is ranked among the very strong El Niño
conditions
• 1991/92 and 2002/2003 seasons were both in the Moderate El Niño
class
• 2014/15 and 2003/04 are among the years classified as Neutral
years
4.2 Impacts on rainfall
Figure 1: Zimbabwe Standardized Precipitation Index (SPI) and Sea
Surface Temperature (SST) anomalies
Results showed that rainfall in Zimbabwe is affected by ENSO
conditions. High sea surface temperature (SST) anomalies, which are
indicative of the El Niño phenomena, often result in negative
standardised precipitation index (SPI). El Niño years are
coinciding with negative SPI values in Zimbabwe. On the other hand,
La Niña years coincide with wet conditions in Zimbabwe.
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Table 3: Categories of rainfall received under different ENSO
events
Above Normal Below Normal Total
El Niño 8 38% 13 62% 21
La Niña 10 67% 5 33% 15
Neutral 13 54% 11 46% 24
60
An analysis of the past 60 years show that the majority of El Niño
years (62%) resulted in below normal rainfall in Zimbabwe. Majority
of La Niña years (67%) result in above normal rainfall in Zimbabwe
while the remaining displayed the opposite (33%).
4.3 Impacts on maize production
An analysis of the maize production trends since 1980 revealed that
production and yield (tonnes per hectares) have been declining
gradually. The period between 2000 and 2016 was characterised by an
increase in area under cultivation even though maize production was
declining. Since maize is the staple food in Zimbabwe, reduced
yields compromise food security in most parts of the country.
Figure 2: National maize production statistics since 1980
.
Figure 3: Maize yield map for the 2015/16 agricultural
season.
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Figure 4: Maize yield map for the 2014/15 agricultural
season.
When the yield values are analysed together with the ENSO
classification, results showed that yield for the different
categories of El Niño events were significantly different. These
statistics assist in understanding the impact of ENSO conditions to
maize yields in Zimbabwe. For the period 1980-2016, El Niño years
have been characterised by lower yields compared to Neutral and la
Niña years at national level. Based on the illustration below,
Masvingo is worst affected by El Niño events compared to other
provinces. All provinces except Mashonaland Central have the best
maize yields during Neutral phase of ENSO.
Figure 5: Provincial maize yield for the different ENSO
classes
Results from the Friedman’s test gave a p-value which is less than
0.05 hence the decision to reject the null hypothesis that there
was no significant difference in maize yield across different ENSO
events in all the provinces. Through a statistical test, there is
evidence that different ENSO events result in wide margins in maize
yields.
Figure 6: Friedman’s test results for different EBSO classes
4.4 Impacts on cattle production Cattle population showed an
increasing or decreasing trend when the country experienced La Niña
and El Niño conditions respectively. Since Very Strong El Niño
conditions often lead to drought, the negative effect on cattle
population is well pronounced with many drought-related cattle
deaths (e.g. 2015/2016 season).
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Figure 7: Cattle Populations for the period 2000-2016
TThe Friedman’s test showed that changes in cattle population due
to ENSO conditions were statistically significant (Figure 8). The p
value was less the 0.05, hence the null hypothesis that there was
no significant difference in cattle populations across different
ENSO events was rejected. Cattle populations across ENSO events are
so different that they can be proven through a statistical
test.
Figure 8: Friedman’s test results on cattle population across
different ENSO classes
4.5 Impacts on water resources Figure 9 below depicts the annual
dam inflow trends (as a %) between 1972 and 2016 plotted against La
Niña, Neutral and El Niño events. Results showed that Neutral and
La Niña were characterised by positive inflows. The strong La Niña
phenomenon experienced in 1974 saw the country experiencing the
highest inflows since 1972. On the other hand, El Niño years
coincided with negative inflows, leading to reduced water in dams
for use by households and communities. It is also worth noting that
the contribution of groundwater has an effect on dam levels figures
in years of water deficit. Figure 10 below show that in most
instances surplus come after years of deficit.
Figure 9: Percentage Inflow for all major dams (1972-2016)
An analysis of the trends on selected ENSO classified years show
that dam levels also respond to ENSO events (Figure 10). This
analysis was done per catchment (Figure 1). Runde catchment was the
worst affected during the El Niño events. For example, during the
2015/16 season, the catchment has the lowest percentage dam levels
in the country. The dam levels trends for individual catchments are
shown in Annex 2.
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Figure 10: Dam level figures per catchment across different ENSO
classes
The Friedman’s test further showed that there was a significant
difference in dam levels in catchments across different ENSO
events. It was thus concluded that different changes in ENSO events
also results in changes in dam levels across the country.
Figure 11: Friedman’s test results for dam levels in different
catchments
4.6 Scenario planning The SST anomalies in the Pacific zone
reflected the occurrence of La Niña conditions. The Southern
African Development Community’s (SADC) Climate Services Centre and
Zimbabwe’s Meteorological Services Department have already issued
out the regional and national seasonal outlook reports for the
2016/17 rainfall season. These outlook reports are also indicating
La Niña conditions. As a result, normal to above normal rainfall is
expected for most parts of the country. Using historical figures in
Zimbabwe, the following table illustrates the three different La
Niña phenomenon as well as Neutral classes and their probable
impacts to dam levels as well as maize and cattle production.
Table 4: Summary of impacts under different La Niña scenarios
La Niña Class Impact on maize production
Impact on cattle population
Impact on dam levels
Neutral Average maize yields
Low water levels for most inland dams.
Weak La Niña Average maize yields
Few deaths due to lack of pastures
Low dam levels
More pastures leading to improved cattle conditions
Average dam levels
Strong La Niña Above average yields due to increased water from
direct rainfall as well as dams
A lot of water for pastures often resulting in waterlogging of low
lands and diseases outbreak due to waterborne pathogens
High dam levels
Given the above summary on the likely impacts under the three La
Niña classes, implications to climate change and resilience
programme are shown in Table 5 below.
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Table 5: Summary of implications to climate change and resilience
programmes in Zimbabwe
ENSO Class
Potential Impact Recommended Interventions
Neutral Fair chances of normal to above rainfall leading to fairly
high maize yields, dam inflows and no negative effects on cattle
populations in the country. Overall verdict: Little or no impact on
programming
1. Improved crop, livestock and agro- forestry production
(climate-smart)
2. Livelihood diversification 3. Small productive infrastructure 4.
Integrated DRM and Resilience
planning at district and ward level 5. Access, control and
sustainable use of
community and household assets 6. Sustainable and equitable
utilisation of
natural resources 7. Integrated water resources management
Weak La Niña
There will be fair chances of normal to above rainfall leading to
fairly high maize yields, dam inflows and no negative effects on
cattle populations in the country. Overall verdict: Little or no
impact on programming
1. Improved crop, livestock and agro- forestry production
(climate-smart)
2. Livelihood diversification 3. Small productive infrastructure 4.
Integrated DRM and Resilience
planning at district and ward level 5. Access, control and
sustainable use of
community and household assets 6. Sustainable and equitable
utilisation of
natural resources 7. Integrated water resources management
Moderate La Niña
More impact on programming with rains supporting crop and livestock
production in most parts of the country
1. Improved crop, livestock and agro- forestry production
(climate-smart)
2. Livelihood diversification 3. Small productive infrastructure 4.
Integrated DRM and Resilience
planning at district and ward level 5. Access, control and
sustainable use of
community and household assets 6. Sustainable and equitable
utilisation of
natural resources 7. Integrated water resources management
Strong La Niña
A lot of rains to support crop, livestock and agro- forestry
production but high chances of flooding in low lands
1. Improved crop, livestock and agro- forestry production
(climate-smart)
2. Livelihood diversification 3. Small productive infrastructure 4.
Integrated DRM and Resilience
planning at district and ward level 5. Access, control and
sustainable use of
community and household assets 6. Sustainable and equitable
utilisation of
natural resources 7. Integrated water resources management
5. CONCLUSION Following the above analysis, the following overall
conclusions can be drawn: The presence of ENSO conditions
significantly influence weather patterns in Zimbabwe. In Zimbabwe,
62% of El Niño events resulted in drier conditions accompanied by
below normal rainfall, usually experienced from October to March.
62% of La Niña was characterized by above rainfall during the rainy
season stretching from October to March.
• Since 1971, 62% of the years which experienced the El Niño
phenomenon, Zimbabwe received below normal rainfall thereby
impacting negatively on dam levels, maize production and cattle
populations. On the other hand, 67% of La Niña conditions have
resulted in above normal rainfall with higher dam levels, maize and
cattle populations compared to El Niño events.
• 54% of the Neutral years have resulted in above rainfall in the
country. These years also saw most provinces receiving higher maize
yields compared to other years due to less chances of either
moisture stress or flooding.
• These trends prove the importance of Sea Surface Temperate (SST)
anomaly figures (which are used to determine ENSO phases) as
possible early warning indicators when planning resilience
programme activities.
• With the 2016/17 climate forecast predicting conditions ranging
between La Niña and Neutral, the scenarios developed anticipate
little to no disruption to resilience programme activities.
However, the developed scenarios also include moderate and strong
La Niña, in case conditions in the Pacific Ocean change. Besides
planning for resilience activities, these scenarios are also useful
for early recovery activities as the country is still recovering
from the Strong El Niño phenomenon of the 2015/2016 agricultural
season.
• All the work presented in this note highlight the strong need for
resilience programme activities to use early warning information,
in the form of ENSO information, for planning purposes. ENSO
phenomenon proved to have a strong bearing on the country’s
rainfall, dam levels, maize and cattle production.
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