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| - | ='''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 '''= | ||
| - | |||
| - | 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 '''= | ||
| - | |||
| - | 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 '''= | ||
Revision as of 09:49, 18 August 2006
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. 
