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('''A simple rainfall map for the current dekad''')
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<blockquote> <blockquote>
 +='''Preparation of ten-daily rainfall and ET<sub>0</sub> maps for crop forecasting '''=
 +
 +Crop forecasting based on water balance calculations is usually done in a ten-day timestep. A ten day period is called a “dekad”. However, should daily weather data of good spatial and temporal extend be available, the water balance can be run in AgrometShell on a daily basis.
 +
 +In order to do crop forecasting the following weather data have to be gathered:
 +* Actual decadal rainfall data for the running season.
 +* Actual decadal ET<sub>0</sub> data for the running season
 +* Normal rainfall data
 +* Normal ET<sub>0</sub> data
 +
 +These data form indicators in itself, even without using them directly in a water balance calculation. Some examples are given below:
 +
='''Preparation of ten-daily rainfall and ET<sub>0</sub> maps for crop forecasting '''= ='''Preparation of ten-daily rainfall and ET<sub>0</sub> maps for crop forecasting '''=
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|width="225"|With the world map as default, some cluttered data are shown for Bangladesh ||[[Image:graph38.jpg|400px|]] |width="225"|With the world map as default, some cluttered data are shown for Bangladesh ||[[Image:graph38.jpg|400px|]]
|--- |---
-|width="225"|Using the zoom buttons an image for just Bangladesh is selected. ||[[Image:graph39.jpg|400px|]] +|width="225"|Using the zoom buttons an image for just Bangladesh is selected. ||[[Image:graph39.jpg|300px|]]
|} |}

Revision as of 09:48, 18 August 2006

Contents

Preparation of ten-daily rainfall and ET0 maps for crop forecasting

Crop forecasting based on water balance calculations is usually done in a ten-day timestep. A ten day period is called a “dekad”. However, should daily weather data of good spatial and temporal extend be available, the water balance can be run in AgrometShell on a daily basis.

In order to do crop forecasting the following weather data have to be gathered:

  • Actual decadal rainfall data for the running season.
  • Actual decadal ET0 data for the running season
  • Normal rainfall data
  • Normal ET0 data

These data form indicators in itself, even without using them directly in a water balance calculation. Some examples are given below:

Preparation of ten-daily rainfall and ET0 maps for crop forecasting

Crop forecasting based on water balance calculations is usually done in a ten-day timestep. A ten day period is called a “dekad”. However, should daily weather data of good spatial and temporal extend be available, the water balance can be run in AgrometShell on a daily basis.

In order to do crop forecasting the following weather data have to be gathered:

  • Actual decadal rainfall data for the running season.
  • Actual decadal ET0 data for the running season
  • Normal rainfall data
  • Normal ET0 data

These data form indicators in itself, even without using them directly in a water balance calculation. Some examples are given below:

Preparation of ten-daily rainfall and ET0 maps for crop forecasting

Crop forecasting based on water balance calculations is usually done in a ten-day timestep. A ten day period is called a “dekad”. However, should daily weather data of good spatial and temporal extend be available, the water balance can be run in AgrometShell on a daily basis.

In order to do crop forecasting the following weather data have to be gathered:

  • Actual decadal rainfall data for the running season.
  • Actual decadal ET0 data for the running season
  • Normal rainfall data
  • Normal ET0 data

These data form indicators in itself, even without using them directly in a water balance calculation. Some examples are given below:

Preparation of ten-daily rainfall and ET0 maps for crop forecasting

Crop forecasting based on water balance calculations is usually done in a ten-day timestep. A ten day period is called a “dekad”. However, should daily weather data of good spatial and temporal extend be available, the water balance can be run in AgrometShell on a daily basis.

In order to do crop forecasting the following weather data have to be gathered:

  • Actual decadal rainfall data for the running season.
  • Actual decadal ET0 data for the running season
  • Normal rainfall data
  • Normal ET0 data

These data form indicators in itself, even without using them directly in a water balance calculation. Some examples are given below:

A simple rainfall map for the current dekad

Start the “Database-Map” function. This example will display rainfall data for a specific dekad in 2002 for Bangladesh.
With the world map as default, some cluttered data are shown for Bangladesh
Using the zoom buttons an image for just Bangladesh is selected.








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