MCP For Claude Marketplace
Irrigation Scheduler

Irrigation Scheduler MCP Connector for Claude

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Calculate precise irrigation needs using the FAO-56 Penman-Monteith model.

4 tools Official Updated Oct 1, 2026 Official Vinkius Partner
More Details Connect to Claude

This MCP server provides precise agricultural water management by implementing the FAO-56 Penman-Monteith evapotranspiration model. It allows AI agents to calculate atmospheric water demand via calculate_et_reference, determine specific crop requirements with calculate_crop_demand, and produce actionable plans using generate_irrigation_schedule. You can also monitor plant health by using check_soil_moisture_status to identify potential water stress risks based on soil capacity and daily demand.

irrigationfarmingevapotranspirationagtechwater-management

4 tools expose this connector's capabilities to your AI agent.

calculate_crop_demand

Calculates the specific water requirement for a given crop type and growth stage

calculate_et_reference

Determines the atmospheric water demand (ETo) based on meteorological data

check_soil_moisture_status

Evaluates if a specific soil moisture level is sufficient to sustain the crop until the next scheduled event

generate_irrigation_schedule

Produces the final actionable irrigation plan including depth, timing, and volume

See how to talk to your AI agent using Irrigation Scheduler.

Calculate the reference evapotranspiration for 25°C, 50% humidity, 2 m/s wind speed, and 15 MJ/m2 solar radiation.

The calculated Reference Evapotranspiration (ETo) is 4.2 mm/day.

What is the crop water demand if the ETo is 5 mm/day and the crop coefficient is 0.8?

The total crop evapotranspiration (ETc) is 4.0 mm/day.

Generate an irrigation schedule for a crop needing 5 mm/day, with 2 mm of effective rainfall, 30 mm soil capacity, and 80% efficiency.

The required irrigation depth is 4.38 mm, with a suggested frequency of 6 days between irrigations, totaling 26.25 mm³ per unit area.

It uses the FAO-56 Penman-Monteith method, which balances atmospheric demand (evapotranspiration) against soil water availability and effective rainfall.

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