Paper Search Console

Home Search Page About Contact

Journal Title

Title of Journal: Theor Appl Climatol

Search In Journal Title:

Abbravation: Theoretical and Applied Climatology

Search In Journal Abbravation:

Publisher

Springer Vienna

Search In Publisher:

DOI

10.1016/0273-1223(95)00594-d

Search In DOI:

ISSN

1434-4483

Search In ISSN:
Search In Title Of Papers:

Developing seasonal rainfall scenarios for food se

Authors: Gregory J Husak Christopher C Funk Joel Michaelsen Tamuka Magadzire Kirk P Goldsberry
Publish Date: 2013/01/30
Volume: 114, Issue: 1-2, Pages: 291-302
PDF Link

Abstract

Rainfed agriculture in SubSaharan Africa accounts for 95  of the local cereal production impacting hundreds of millions of people Early identification of poor rainfall conditions is a critical indicator of food security As such monitoring accumulated seasonal rainfall gives an important midseason estimate of final accumulated totals However characterizing the remaining uncertainty in a season has largely been ignored by the food security community This paper presents a new technique describing rainfall conditions over the duration of a cropgrowing cycle by combining estimated rainfalltodate with potential scenarios for the remaining season based on available satellite rainfall estimates the common tool for rainfall analysis in Africa The limited historical record provided by satellite rainfall estimates using previous seasons provides only a coarse view of likely seasonal totals To combat this scenarios developed by bootstrapping dekadal data to create synthetic seasons allow for a finer understanding of potential seasonal accumulations Updating this throughout the season shows a narrowing envelope of seasonal totals converging on the final seasonal result The resulting scenarios inform the expectations for the final seasonal rainfall accumulation allowing analysts to quantify and visualize the uncertainty in seasonal totals Giving decision makers a tool for understanding the likelihood of specific rainfall amounts provides additional time to enact and mobilize efforts to reduce the impact of agricultural droughtMuch of the developing world relies heavily on rainfed agriculture In SubSaharan Africa rainfed farms account for 95  of the local cereal production Wani et al 2009 employing 70  of the people Gelb and World Bank 2000 Wani et al 2009 When widespread drought strikes crops millions of people mostly women and children face hunger Such was the case in 2009 when poor rainfall contributed to an increase of 53 million foodinsecure people in SubSaharan Africa according to the annual “State of Food Insecurity in the World” publications by FAO Food and Agriculture Organization of the United Nations 2008 2009 Fortunately effective early warning in 2009 helped to provoke effective food aid responses totaling 36 million metric tons1 Effective and early rainfall monitoring based on satellite rainfall estimates Funk et al 2003 Artan et al 2007 plays an important role in guiding humanitarian responses These estimates while imperfect Dinku et al 2008 capture the spatial patterns of rainfall and can be compared against previous years to identify anomalous rainfall Funk and Verdin 2009 As the satellite record increases with time there is a more robust archive of estimates to compare with current values Exploiting this historical information effectively can lead to more accurate and timely drought early warning saving lives and livelihoods and limiting the economic disruptions produced by extreme weather This paper attempts to combine crop phenology information and satellitebased rainfall estimates to quantify cropspecific rainfall accumulations in a probabilistic framework Monitoring rainfall over the course of the growing cycle of a crop provides a proxy for crop performance that can be compared to other seasons in the satellite record Generating endofseason results using rainfall from previous years to fill out a season helps to define both the expectation and variability in the remainder of the cropgrowing season This variability gives a sense for the uncertainty related to the estimated expectation an important element for decision makers to determine the appropriate responseThe following section describes the rainfall estimates and how the season is parameterized using this rainfall Then a brief evaluation of seasonal rainfall totals based on the satellite rainfall record is described for Southern Africa highlighting regimes prone to rainfallrelated crop yield reductions Section 3 details the scenario monitoring technique with an example from the 2009–2010 growing season for Southern Africa The results are displayed through a series of maps presenting different characterizations based on the scenario analysis Section 4 steps through the season for a single administrative zone of Zimbabwe capturing the narrowing cone of uncertainty includes a validation of the technique by comparing endofseason conditions to the forecast range developed in midseason and raises potential issues going forward The final section summarizes the major findings and potential applications of this researchCurrent estimates show that nearly 160 million people are undernourished in SubSaharan Africa Food and Agriculture Organization of the United Nations 2011 In Southern Africa more than one in three people face undernourishment Food aid to SubSaharan Africa in 2010 accounted for nearly twothirds of all global food aid with 72  of the received amount coming in the form of “Emergency Aid” World Food Programme 2011 Providing tools for analysis to inform decisions regarding the correct amount of aid and timeframe for delivery to prevent undernourishment can directly impact millions of livesThe analyses presented in this report are based on the National Oceanic and Atmospheric Administration NOAA satellite rainfall estimates RFE2 Xie and Arkin 1997 The RFE2 integrates daily rainfall observations geostationary infrared cold cloud duration rainfall fields and passive microwave rainfall retrievals to produce 01° daily grids of rainfall for Africa While satellite rainfall fields are associated with significant bias in areas of complex terrain Dinku et al 2008 this bias can be reduced using highresolution climatologic rainfall fields Funk et al 2007 to track agricultural crop water deficits Funk and Verdin 2009 Furthermore in areas without much complex topography such as Zimbabwe the RFE2 has been shown to be a preferred rainfall estimate Dinku et al 2008 The RFE2 drives a number of monitoring products used in the food security analysis such as the standardized precipitation index SPI and water requirement satisfaction index WRSI The ability to use RFE2 for quantitatively monitoring food security in Africa is affirmed in literature Tadross et al 2005 Verdin et al 2005 Sawunyama and Hughes 2008 Tadesse et al 2008Algorithms exist to utilize RFE2 data to establish some seasonal parameters for Africa Onset of rains establish the start of season SOS for each location Detection of SOS for Southern Africa begins in September which is the earliest possible planting date This research uses the technique developed in West Africa AGRHYMET 1996 and reinforced in WRSI literature Verdin and Klaver 2002 Senay and Verdin 2003 defining SOS as the first dekad receiving 25 mm of rainfall followed by two dekads summing to 20 mm While there may be local deviations from this as a viable SOS it is a widely supported approximation Tadross et al 2005 Tadesse et al 2008 Funk and Budde 2009 Crespo et al 2011 Harrison et al 2011The WRSI is a measure of the fraction of the water demand of a crop that is being met by soil moisture and rainfall Frere and Popov 1986 Senay and Verdin 2003 Verdin and Klaver 2002 The WRSI incorporates components of rainfall potential evapotranspiration and soil moisture Additionally a crop coefficient specific to the crop type determines the water demand of the crop for the phonological cycle from the SOS for the entire LGP The WRSI is a leading indicator of crop yield in monitoring African food production and is therefore a logical product to use in defining growing season characteristics for this study It should be noted that for many regions there is a good correspondence between seasonal rainfall totals what this study investigates and end of season WRSI values Verdin et al 2005


Keywords:

References


.
Search In Abstract Of Papers:
Other Papers In This Journal:

  1. Investigation of temporal-spatial parameters of an urban heat island on the basis of passive microwave remote sensing
  2. Weather maps classification over Greek domain based on isobaric line patterns
  3. Stable estimations for extreme wind speeds. An application to Belgium
  4. Retrieving daily global solar radiation from routine climate variables
  5. Soil moisture variations in remotely sensed and reanalysis datasets during weak monsoon conditions over central India and central Myanmar
  6. On the consideration of mesoscale transports in climate modelling
  7. A hybrid SVM-FFA method for prediction of monthly mean global solar radiation
  8. Regional droughts in southern South America
  9. High temperature extremes in the Czech Republic 1961–2010 and their synoptic variants
  10. Trends, time-varying and nonlinear time series models for NGRIP and VOSTOK paleoclimate data
  11. Estimation of daily global solar radiation as a function of routine meteorological data in Mediterranean areas
  12. North Sea near-surface wind climate and its relation to the large-scale circulation patterns
  13. A sensitivity study on the role of the swamps of southern Sudan in the summer climate of North Africa using a regional climate model
  14. On the link between potential evaporation and regional evaporation from a CBL perspective
  15. Evaluation of six parameterization approaches for the ground heat flux
  16. Identification of the principal patterns of summer moisture transport in South America and their representation by WCRP/CMIP3 global climate models
  17. Long-term snow and weather observations at Weissfluhjoch and its relation to other high-altitude observatories in the Alps
  18. Analysis of monthly, winter, and annual temperatures in Zagreb, Croatia, from 1864 to 2010: the 7.7-year cycle and the North Atlantic Oscillation
  19. Low-frequency sea-level variability in the South China Sea and its relationship with ENSO
  20. Climatology of Alaskan wildfires with special emphasis on the extreme year of 2004
  21. Large-scale climate variability and its effects on mean temperature and flowering time of Prunus and Betula in Denmark
  22. Synoptic reasons for heavy snowfalls in the Polish – German lowlands
  23. Study of evapotranspiration and evaporation beneath the canopy in a buckwheat field
  24. Climate change scenarios of precipitation extremes in Central Europe from ENSEMBLES regional climate models
  25. Simulation skill of APCC set of global climate models for Asian summer monsoon rainfall variability
  26. Trends of temperature and precipitation extremes in the Loess Plateau Region of China, 1961–2010
  27. Enhanced temperature variability in high-altitude climate change
  28. Dependency of typhoon intensity and genesis locations on El Niño phase and SST shift over the western North Pacific
  29. Seasonal variation of the ITCZ and its characteristics over central Africa
  30. Multischeme ensemble forecasting of surface temperature using neural network over Turkey
  31. North–south differences in Chinese agricultural losses due to climate-change-influenced droughts
  32. 1/f noise in the UV solar spectral irradiance
  33. Assessment of the impacts of climate change and brackish irrigation water on rice productivity and evaluation of adaptation measures in Ca Mau province, Vietnam
  34. Validation of TRMM Precipitation Radar satellite data over Indonesian region
  35. Vertical characteristics of cyclonic tracks over the eastern Mediterranean during the cold period of the year
  36. The influence of atmospheric circulation on the intensity of urban heat island and urban cold island in Poznań, Poland
  37. Uncertainty analysis of statistically downscaled temperature and precipitation regimes in Northern Canada
  38. Connection between the genesis number of tropical cyclones over the western North Pacific and summer rainfall over Northeast Asia
  39. Relative role of pre-monsoon conditions and intraseasonal oscillations in determining early-vs-late indian monsoon intensity in a GCM
  40. An observational study of the summer Mediterranean Sea breeze front penetration into the complex topography of the Jordan Rift Valley
  41. Variability of tropical days over Greece within the second half of the twentieth century
  42. Evaluating rainfall patterns using physics scheme ensembles from a regional atmospheric model
  43. European winter precipitation extremes and large-scale circulation: a coupled model and its scenarios
  44. Analysis of multidimensional aspects of agricultural droughts in Zimbabwe using the Standardized Precipitation Index (SPI)
  45. Comparison of intra-seasonal forecast of Indian summer monsoon between two versions of NCEP coupled models
  46. UV irradiance on arbitrarily oriented surfaces: variation with atmospheric and ground properties
  47. Spatial and temporal aspects of the lake effect on the southern shore of Lake Superior
  48. Climate change may already threaten Scots pine stands in the Swiss Alps
  49. The surface energy budget and interannual variation of the annual total evaporation over a highland lake in Southwest China
  50. Multi-sensor for measuring erythemally weighted irradiance in various directions simultaneously
  51. Influence of non-feedback variations of radiation on the determination of climate feedback
  52. Distribution of convective energy at upper level in South Korea and the possibility of artificial showery rain caused by activated CAPE
  53. Characteristics of large-scale atmospheric circulation related to extreme monthly rainfall anomalies in the Pampa Region, Argentina, under non-ENSO conditions

Search Result: