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🗺️Drought, Climate Classification & Agro-Climatic Zones of India

Drought types and agricultural drought sub-types, weather forecasting, 15 agro-climatic zones, 20 agro-ecological regions, Koppen and Thornthwaite classification, LGP, and meteorological institutions and instruments

Why Drought and Climate Zones Matter for Agriculture

In the previous lesson, we explored clouds and cloud seeding — how clouds form, the 10 types, and artificial rainmaking techniques. Now we tackle the consequences when rain fails: drought — and the classification systems that help planners match crops to regions.

In 2018, a severe drought in Maharashtra forced thousands of farmers to abandon their soybean and cotton crops. Dryland farmers in Rajasthan routinely face crop failure when growing periods shrink below 5 weeks. Understanding drought classification helps design contingency plans, while knowing India’s agro-climatic zones ensures that the right crop is grown in the right region — the foundation of agricultural planning.

This lesson covers:

  1. Drought types — meteorological, agricultural, hydrological, socio-economic
  2. Agricultural drought sub-types — early, mid, late, chronic, apparent
  3. Drought indices — AAI, MAI, MDI, NDVI, SPI, Palmer Index
  4. Weather forecasting — short, medium, and long range; synoptic vs statistical methods
  5. IMD and agro-meteorological services — AMD, IAAS, DAAS, AMFUs
  6. Growing Degree Days and crop-weather models — GDD formula, CERES, DSSAT
  7. Length of Growing Period — LGP thresholds for cropping systems
  8. Agro-climatic zones — Planning Commission’s 15 zones, ICAR’s 127 zones, NBSS&LUP’s 20 AERs
  9. Climate classification — Koppen, Thornthwaite, Troll systems
  10. Meteorological instruments — heights, uses, and key devices

All topics are high-yield for IBPS AFO, NABARD, and ICAR-JRF exams.


What is Drought?

Drought can be defined in three ways:

  1. The condition under which crops fail to mature because of insufficient water supply through rains.
  2. A situation where water required for transpiration and evaporation by crops exceeds available soil moisture.
  3. No precipitation in a rainy season for more than 15 days continuously — such stretches are called dry spells.

IMPORTANT

Droughts are classified into 4 main categories that occur in a cascading sequence: Meteorological → Agricultural → Hydrological → Socio-economic.


Four Types of Drought

TypeDefinitionKey ThresholdAgricultural Impact
MeteorologicalSeasonal rainfall falls below 75% of the climatologically expected normal over a wide areaModerate: 26–50% deficit; Severe: >50% deficitCropping pattern disrupted; sowing delayed
AgriculturalInadequate rainfall followed by soil moisture deficit; 4 consecutive weeks (May–mid Oct) or 6 weeks (rest of year) without adequate soil moistureYield reduction due to soil moisture shortageGrowth reduction; yield loss; crop failure
HydrologicalStreams, rivers, reservoirs, lakes, and wells dry up due to marked depletion of surface water; ground water table fallsLags meteorological drought by weeks/monthsIrrigation sources fail; industry and power affected
Socio-economicDrought impacts on livelihoods, food supply, and economy; cascading effect of the above three typesHuman welfare indicators declineFood prices rise; migration; employment loss; famine

TIP

Cascading sequence for exams: Meteorological → Agricultural → Hydrological → Socio-economic. Agricultural drought is further divided into 5 sub-types (see below).


Five Types of Agricultural Drought

Sub-TypeWhen It OccursCauseAgricultural Example
1. Early SeasonStart of seasonDelayed onset of monsoon or prolonged dry spell after onsetSeedling mortality in rainfed sorghum; need for resowing bajra
2. Mid-SeasonDuring crop growthInadequate soil moisture between two successive rainfall eventsMaize at tasseling stage suffers; grain filling reduced in rice
3. Late Season (Terminal)End of seasonEarly cessation of monsoon; weak monsoon activityRainfed rice in dry sub-humid regions fails due to September rain failure (40–50% dry spells > 5 days)
4. ChronicMost yearsRainfall and stored soil moisture inadequate most yearsAssured growing period is hardly 6–7 weeks in arid Rajasthan; only short-duration bajra survives
5. ApparentAny timeMis-matching of cropping pattern with rainfall/moistureGrowing long-duration rice in a 90-day LGP zone

TIP

Mnemonic — “EML-CA”: Early, Mid, Late (terminal), Chronic, Apparent. These five sub-types cover all agricultural drought scenarios.


Key Drought Terms

TermDefinition
Drought yearAnnual rainfall ≤ 75% of normal
Drought-prone areaSevere or moderate drought in ≥ 20% of years
Chronic drought areaSevere or moderate drought in ≥ 40% of years
Palmer Drought IndexGiven by Palmer (USA, 1965); uses temperature + rainfall to estimate relative soil moisture

Drought and Moisture Indices

IndexFull Form / FormulaUse
AAI (Aridity Anomaly Index)Departure from normal aridityUsed by IMD weekly to monitor agricultural drought in real-time
MAI (Moisture Availability Index)P (at 50% probability) / PET × 100Crop planning in dryland areas
MDI (Moisture Deficit Index)(P − PET) / PET × 100Estimate dryness of a region (used in ICAR classification)
TMI (Thornthwaite Moisture Index)AET / PETHow well water supply meets atmospheric demand
NDVI (Normalised Difference Vegetation Index)Satellite-derived; lower values = stressed vegetationDrought severity assessment from vegetation greenness
SPI (Standardised Precipitation Index)Based solely on monthly precipitation dataVersatile drought index; works across all time scales

TIP

For exams: AAI = IMD weekly drought monitoring. MAI = dryland crop planning. NDVI = satellite-based. SPI = precipitation-only index.


Drought Monitoring Systems

SystemFull FormLocationFunction
NADAMSNational Agricultural Drought Assessment and Monitoring SystemNRSA, DehradunSatellite-based vegetation monitoring using NDVI
NRSANational Remote Sensing AgencyHyderabadRemote sensing data for crop and drought monitoring

NOTE

NADAMS uses satellite-derived NDVI to classify drought severity — lower NDVI values indicate stressed or sparse vegetation, confirming drought conditions.


Weather Forecast Types

Drought monitoring is reactive — it tells us what has happened. Weather forecasting is proactive — it gives farmers advance warning to protect crops. Accurate weather forecasting is the first line of defence against drought and weather damage:

Forecast TypeValidity PeriodPrimary UsersWhat It Predicts
Short rangeUp to 72 hoursFarmers, marine agencies, publicRainfall, heavy rain, heat/cold waves, thunderstorms
— Now casting0–2 hoursSame as aboveImmediate weather conditions
— Very short range0–12 hoursSame as aboveNear-term weather
Medium range3 to 10 daysFarmersRainfall occurrence, temperature trends
Long rangeBeyond 10 days up to a month/seasonPlanners, policy makersMonsoon rainfall; expressed as deviation from normal

NOTE

Daily weather forecast in India is issued from Pune (IMD headquarters). Medium-range forecasts help farmers decide irrigation scheduling, while long-range forecasts help planners allocate seed and fertiliser.

Forecasting Methods

MethodBest ForApproach
SynopticShort-range forecastsWeather maps, pressure systems, fronts
StatisticalShort and long range forecastsHistorical data, statistical relationships

IMD and Agro-Meteorological Services

Agricultural Meteorology Division (AMD)

  • Established at Pune in 1932 — one of the oldest agro-met services worldwide.
  • Services: GKMS (Gramin Krishi Mausam Seva), Agromet advisories, Training for AMFUs.

Integrated Agro-meteorological Advisory Service (IAAS)

MilestoneYearDetail
Weather broadcasts for farmers1945IMD radio broadcasts
State-level advisories1976Short-range forecast based
NCMRWF established1988Medium-range (3–10 day) numerical weather prediction
AMFUs created130 units across all 127 agroclimatic zones in SAUs/ICAR/IITs
IAAS launched1 April 2007IMD took over Agromet Advisory Service
DAAS launched2008District-level Agromet Advisory Service
  • IMD issues 5-day district-level forecasts twice a week using Multi-Model Ensemble technique.
  • Seven parameters: rainfall, max/min temperature, wind speed/direction, RH, cloudiness.
  • Advisories reach farmers through SMS, mobile apps, radio, TV, newspapers, Kisan Call Centres.

TIP

Exam tip: AMD = Pune, 1932. IAAS = 1 April 2007. DAAS = 2008. AMFUs = 130 units.


Growing Degree Days (GDD)

Weather forecasts predict what is coming; Growing Degree Days help predict where a crop stands in its development cycle. GDD is one of the most important tools in agricultural meteorology for predicting crop development and planning farm operations.

  • Formula: GDD = (Tmax + Tmin) / 2 − Tbase
  • Negative values are treated as zero (plants do not undergo negative growth).
  • Base temperature = temperature below which plant growth is zero (e.g., 5°C for cereals).
  • GDDs are accumulated daily from the beginning of the season.
  • Used to compare growing season progress against long-term average and estimate maturity.

IMPORTANT

GDD is frequently asked as a formula question. Remember: negative GDD = zero, and base temp for cereals = 5°C.


Crop-Weather Modelling

Mathematical equations explaining crop interaction with environment, used to predict growth and yield. First used by Baier (1979).

ModelFull FormApplication
CERESCrop Environment Resource SynthesisRice, Maize, Sorghum, Wheat simulation
DSSATDecision Support System for Agro-technology TransferClimate change impact on rice (TN)
PRECISProviding Regional Climates for Impacts StudiesRegional climate projections
InfoCrop-RICEImpact of high temp + elevated CO₂ on rice yield
CROPGRO-GroundnutClimate change impact on groundnut (Anantapur, Junagadh)

TIP

For exams: Baier (1979) = pioneer of crop-weather modelling. CERES = most versatile crop simulation model.


Length of Growing Period (LGP)

LGP is the period when moisture availability from rainfall exceeds half the potential evapotranspiration (PET). It determines what cropping system is viable:

LGP and Cropping System

LGP (Days)Viable Cropping SystemAgricultural Example
< 75Perennial vegetation onlyRangelands in western Rajasthan
75–140Sole croppingSingle crop of bajra or short-duration pulses
140–180IntercroppingSorghum + pigeonpea intercrop in Maharashtra
> 180Double croppingRice-wheat system in Punjab

LGP and Climate Region

LGP (Days)Region
< 75Arid
75–120Semi-Arid
> 120Humid

IMPORTANT

LGP is the single most important parameter for deciding cropping intensity. Regions with LGP < 75 days are too dry for annual crops.


15 Agro-Climatic Zones of India (Planning Commission, 1989)

The Planning Commission of India (1989) divided the country into 15 agro-climatic regions based on rainfall, temperature, topography, cropping systems, and water resources.

All 15 Agro-Climatic Zones — Detailed

1. Western Himalayan Zone

FeatureDetail
StatesJ&K, Himachal Pradesh, UP hills
ClimateCool and humid
Rainfall750–1500 mm
TemperatureJuly: 5–30°C; January: -5 to 5°C
SoilsSkeletal, podsolic, hilly brown; silty loams prone to erosion
CropsWinter: barley, oats, wheat; Kharif: rice (valleys), maize (hills)
HorticultureApple, peach, apricot, pear, cherry, almond, litchi, walnut
SpecialSaffron grown here; cropping intensity lowest in J&K, highest in HP

2. Eastern Himalayan Zone

FeatureDetail
StatesSikkim, Darjeeling, Arunachal Pradesh, NE states, parts of WB
ClimateHumid and sub-humid
Rainfall1840–3530 mm
CropsRice, maize, potato, tea
SpecialShifting cultivation (Jhuming) in ~1/3 of cultivated area; major constraint: soil erosion

3. Lower Gangetic Plains Zone

FeatureDetail
StatesWest Bengal (lower Gangetic plain), Brahmaputra valley
ClimateMoist humid to dry humid
Rainfall1300–1600 mm
SoilsMostly alluvial; flood-prone
CropsRice (main), jute, rapeseed, wheat

4. Middle Gangetic Plains Zone

FeatureDetail
States12 districts of eastern UP, 27 districts of Bihar
Area16 million hectares
Irrigation39% of gross cropped area
Cropping intensity142%
Rainfall1211–1470 mm
CropsSugarcane, paddy, maize, wheat

5. Upper Gangetic Plains Zone

FeatureDetail
States32 districts of central and western UP
Irrigation intensity131% (canals and tube wells)
Cropping intensity145%
Rainfall720–980 mm
CropsRice, wheat, sugarcane

6. Trans-Gangetic Plains Zone

FeatureDetail
StatesPunjab, Haryana, Delhi, Chandigarh, Sriganganagar (Rajasthan)
Also calledSatluj Yamuna Plains
ClimateSemi-arid
Rainfall650–1250 mm
Key distinctionHighest net sown area, highest irrigated area, high cropping intensity, highest ground water utilisation
CropsWheat, sugarcane, cotton, rice, gram, maize, pulses, oilseeds

7. Eastern Plateau and Hills Zone

FeatureDetail
StatesEastern MP, southern WB, most of inland Odisha
ClimateMoist sub-humid to dry sub-humid
Rainfall1270–1435 mm
SoilsRed, yellow, laterites, alluvium; shallow to medium depth
IrrigationThrough tanks and tube wells
CropsRice, millets, maize, oilseeds, ragi, gram, potato
SpecialLargest agro-climatic zone in India; deficient in water resources

8. Central Plateau and Hills Zone

FeatureDetail
States46 districts of MP, parts of UP and Rajasthan
ClimateSemi-arid to dry humid
Rainfall400–1550 mm
Rainfed area75% with low-value cereal crops
SoilsMixed red, yellow, black; ravines present
CropsWheat, gram, jowar, bajra, paddy, millets, oilseeds, cotton
ConstraintScarcity of water

9. Western Plateau and Hills Zone

FeatureDetail
StatesMajor part of Maharashtra, parts of MP, one district of Rajasthan
ClimateSemi-arid
Rainfall600–1040 mm (avg 904 mm)
Irrigated areaOnly 12.4%
SoilsRegur (black) soil
CropsJowar, bajra, cotton, wheat
SpecialProvides 50% of India’s jowar; best quality orange, grape, and banana

10. Southern Plateau and Hills Zone

FeatureDetail
States35 districts of AP, Karnataka, and TN
ClimateSemi-arid
Dryland farming81% of area
Cropping intensity111%
Rainfall675–1000 mm
CropsCoffee, cotton, tea, cardamom, spices

11. East Coast Plains and Hills Zone

FeatureDetail
StatesEast coast of TN, AP, and Odisha
ClimateSemi-arid and dry sub-humid
Rainfall780–1290 mm
SoilsAlluvial and coastal sands
Rainfed area75%
CropsRice, ragi, jowar, bajra
SpecialContributes 17.5% of India’s groundnut production

12. West Coast Plains and Ghats Zone

FeatureDetail
StatesWest coast of TN, Kerala, Karnataka, Maharashtra, Goa
Rainfall2230–3650 mm (highest rainfall zone)
SoilsLaterite and coastal alluvial
CropsRice, ragi, groundnut, tapioca
SpecialSpices and plantation crops along Western Ghats hill slopes

13. Gujarat Plains and Hills Zone

FeatureDetail
States19 districts of Gujarat
ClimateArid and semi-arid
Irrigated areaOnly 32.5%
Rainfed area78%; about 60% drought-prone
Rainfall340–1793 mm
CropsMaize, wheat, groundnut, tobacco, cotton, jowar, bajra
SpecialKnown as “Oilseed Region”

14. Western Dry Zone

FeatureDetail
StatesNine districts of Rajasthan
CharacteristicsHot sandy desert; erratic rainfall; scanty vegetation; no perennial rivers
Rainfall95 mm (lowest in India)
Ground waterDeep and often brackish
Forest area1.2%; irrigated: 6.3%
Cropping intensity105% (lowest)
CropsBajra, gram, wheat, rapeseed
SpecialFamine and drought are common features

15. Islands Zone

FeatureDetail
StatesAndaman & Nicobar Islands and Lakshadweep
ClimateEquatorial
Rainfall3000 mm over 8–9 months
CropsRice, maize, millets, pulses, arecanut, turmeric, cassava
SpecialNearly half the cropped area under coconut

Key Zone Facts for Exams

ZoneDistinguishing Feature
Trans-Gangetic (Zone 6)Highest net sown area, highest irrigated area, highest cropping intensity, highest groundwater use
Eastern Himalayan (Zone 2)Shifting cultivation (Jhuming)
Eastern Plateau & Hills (Zone 7)Largest agro-climatic zone
Gujarat Plains (Zone 13)Oilseed zone; 60% drought-prone
Western Plateau (Zone 9)50% of India’s jowar; best orange, grape, banana
Western Dry (Zone 14)Lowest rainfall (95 mm); famine and drought zone
West Coast (Zone 12)Highest rainfall (2230–3650 mm)
Western Himalayan (Zone 1)Saffron cultivation

ICAR Classification — 127 Agro-Climatic Zones (NARP)

Under the National Agricultural Research Project (NARP), ICAR advised State Agricultural Universities to divide each state into sub-zones based on rainfall, cropping pattern, and administrative units. This yielded 127 agro-climatic zones. ICAR’s climate classification uses Moisture Deficit Index (MDI) under the All India Coordinated Research Project on Dryland Agriculture, specifically designed for agricultural planning in dryland areas.

State-wise NARP Zones (Selected)
StateZonesStateZones
Madhya Pradesh12 (most)Uttar Pradesh10
Karnataka10Rajasthan9
Odisha9Maharashtra9
Gujarat8Kerala8
Andhra Pradesh7Tamil Nadu7
West Bengal6Assam6
Bihar6NE Hill region6
Punjab5J&K4
Himachal Pradesh4Haryana2

Key Numbers for Exams

ClassificationNumberAuthority
Agro-climatic regions (Planning Commission)15Planning Commission, 1989
Agro-climatic zones (NARP)127ICAR/NARP
Total ACZs (ICAR reclassification)131ICAR
Agro-ecosystems under NARP5ICAR
Agro-ecological regions (NBSS&LUP)20NBSS&LUP/ICAR
State with most NARP zonesMadhya Pradesh (12)ICAR

20 Agro-Ecological Regions (NBSS & LUP)

The National Bureau of Soil Survey and Land Use Planning (NBSS & LUP) of ICAR delineated 20 agro-ecological regions (AERs) using the FAO 1978 concept — superimposing length of growing periods and bio-climate maps on soil physiographic maps.

All 20 Agro-Ecological Regions
EcosystemNo.RegionKey StatesEco-regionSoil Type
Arid1Western HimalayaJ&K, HPCold AridShallow skeletal
Arid2Deccan PlateauAP, KarnatakaHot AridRed & Black
Arid3Western Plain, Kutch, part of KathiawarGujarat, Rajasthan, Haryana, PunjabHot AridDesert & Saline
Semi-Arid4Northern Plain & Central Highlands (Aravallis)Gujarat, Rajasthan, UP, MP, Haryana, PunjabHot Semi-AridAlluvium Derived
Semi-Arid5Central (Malwa) Highlands, Gujarat PlainsGujarat, MPHot Semi-AridMedium & Deep Black
Semi-Arid6Deccan PlateauKarnataka, AP, Maharashtra, MPHot Semi-AridShallow & Medium Black
Semi-Arid7Deccan (Telangana) Plateau & Eastern GhatsAPHot Semi-AridRed and Black
Semi-Arid8Eastern Ghats, TN Uplands, Deccan (Karnataka) PlateauKarnataka, TN, KeralaHot Semi-AridRed Loamy
Sub-Humid9Northern PlainBihar, UP, PunjabHot Sub-humid (dry)Alluvium-derived
Sub-Humid10Central Highlands (Malwa, Bundelkhand, Eastern Satpura)MP, MaharashtraHot Sub-humidBlack & Red
Sub-Humid11Eastern Plateau (Chhattisgarh)MPHot Sub-humidRed & Yellow
Sub-Humid12Eastern Plateau (Chhota Nagpur) & Eastern GhatsOdisha, WB, Bihar, MP, MaharashtraHot Sub-humidRed & Laterite
Sub-Humid13Eastern PlainUP, BiharHot Sub-humid (moist)Alluvium-derived
Sub-Humid14Western HimalayasJ&K, HP, UPWarm Sub-humid to humidBrown Forest & Podzolic
Humid/Per-humid15Bengal & Assam PlainsWB, AssamHot Sub-humid to HumidAlluvium derived
Humid/Per-humid16Eastern HimalayasArunachal Pradesh, Sikkim, WBWarm Per-humidBrown & Red Hill
Humid/Per-humid17NE Hills (Purvanchal)Tripura, Mizoram, MeghalayaWarm Per-humidRed & Lateritic
Coastal18Eastern Coastal PlainTN, Puducherry, AP, Odisha, WBHot Sub-humid to Semi-aridCoastal Alluvium
Coastal19Western Ghats & Coastal PlainKerala, Goa, Maharashtra, GujaratHot Humid Per-humidRed, Lateritic, Alluvium
Island20Andaman-Nicobar & LakshadweepA&N, LakshadweepHot Humid Per-humidRed Loamy & Sandy

AER Ecosystem Distribution

Ecosystem TypeNumber of AERs
Arid3
Semi-Arid5
Sub-Humid6
Humid/Per-humid3
Coastal2
Island1
Total20

Climate Classification Systems

Agro-climatic zones are practical divisions for planning. Climate classification systems provide the scientific framework behind those divisions. Different scientists have classified climate using different criteria:

Classification ByBasisKey Detail
De CandolleVegetationEarliest; plant-based
Koppen (1884, modified 1918, 1936)Mean monthly temperature and mean annual rainfallMost widely used; first quantitative classification; 5 groups
Thornthwaite (1931)P/E ratio and P/E index (sum of 12 monthly P/E ratios)Recognised runoff and percolation losses; 6 temperature provinces (Tropical to Frost)
Thornthwaite and Mather (1948)Moisture index (Im), PETIm = 100 × [(P − PE) / PE]; modified by Mathur (1955)
Troll (1965)Temperature and duration of humid monthsClassification called “Seasonal Climates of the Earth”; humid month = month where P > PET; modified by ICRISAT for India

Koppen Classification (A, B, C, D, E)

Koppen divided climate into five categories:

GroupClimate TypeTemperature/Precipitation CriteriaIndian Agricultural Region
ATropical rainyCoolest month > 18°C; P > EKerala, coastal Karnataka — rice, coconut, spices
BTropical dryCoolest month > 18°C; P < ERajasthan, Gujarat — bajra, guar, drought-tolerant crops
CHumid temperate rainyCoolest month 18°C to -3°CNilgiris, Western Ghats hills — tea, coffee
DCold forestCoolest month < -3°C; precipitation as snowKashmir, HP — apple, walnut, saffron
EPolarWarmest month < 10°CLadakh — minimal agriculture

TIP

Exam fact: Groups A, C, D, E are classified based on temperature. Group B is the only one classified based on rainfall (precipitation vs evaporation).


Thornthwaite Classification — Moisture Index (Im)

Im ValueClimateAgricultural Viability
100 and abovePer humidPlantation crops; waterlogging risk
20 to 100HumidRice, jute, tea
0 to 20Moist sub-humidWheat, maize with some irrigation
-33.3 to 0Dry sub-humidRainfed millets, pulses
-66.7 to -33.3Semi-aridSorghum, groundnut, cotton
-100 to -66.7AridOnly drought-tolerant crops with irrigation

Moisture Deficit Index formula: MDI = 100 (P - PET) / PET

NOTE

Thornthwaite classified climate based on PE index, TE index, and seasonal distribution of rainfall. Optimum years of weather data for defining climate: 31 years.


Meteorological Institutions

The classification systems above were developed by international scientists, but India’s own meteorological infrastructure implements them. These institutions and their founding details are frequently asked in exams.

InstitutionLocation & YearKey Function
IMO (International Meteorological Organization)Geneva, 1873Predecessor of WMO
IMD (Indian Meteorological Department)Calcutta, 1875 (later Shimla → Pune → New Delhi)India’s weather forecasting authority
WMO (World Meteorological Organization)Switzerland, 1950Global weather coordination
IITM (Indian Institute of Tropical Meteorology)Pune, 1962Monsoon and tropical weather research
IIRS (Indian Institute of Remote Sensing)Dehradun, 1966Remote sensing for agriculture
NCMRWFNew Delhi, 1988Medium range weather forecasting
NRSA (National Remote Sensing Agency)HyderabadSatellite-based crop monitoring

WARNING

Common exam confusion: IMO (1873, Geneva) is the predecessor of WMO (1950). IMD was established in Calcutta in 1875, not Pune or Delhi (those were later shifts).


Agro-Meteorological Observatory Standards

StandardSpecification
Distance from buildings/trees10 times the height of the obstacle
Plot size60 m (N-S) x 40 m (E-W)

Meteorological Instruments — Heights and Uses

Every agro-meteorological observatory follows standardised placement rules to ensure consistent, comparable data. The heights below and the instrument-function pairings are heavily tested in competitive exams.

Standard Heights from Ground Level

InstrumentHeightWhat It Measures
Sunshine recorder, Anemometer, Wind vane3.08 mSunshine hours, wind speed, wind direction
Stevenson screen1.22 mHouses thermometers (max, min, dry/wet bulb)
Automatic rain gauge75 cmContinuous rainfall recording
Ordinary rain gauge, Evaporation pan50 cmDaily rainfall, evaporation

Key Instruments and Their Uses

InstrumentMeasuresAgricultural Use
IR Gun / Infrared ThermometerPlant canopy surface temperature (8–14 μm range)Estimates crop water stress without contact
Net RadiometerNet radiation at earth’s surfaceEnergy balance studies
Quantum SensorPAR above crop canopyLight availability for photosynthesis
Tube SolarimeterPAR reaching ground through crop canopyCanopy light interception efficiency
PyradiometerBoth long-wave and short-wave radiationTotal radiation balance studies
Assaman PsychrometerRH in open and crop canopyHumidity monitoring for pest management
HygrographContinuous record of RHLong-term humidity tracking
Rain GaugeRainfallBasic rainfall measurement
PluviographContinuous rainfall recordRainfall intensity analysis
Drosometer / Dew GaugeDew measurementDew contribution to dryland crops
USWB Evaporimeter / AtmometerEvaporationIrrigation scheduling
Cone PenetrometerSoil mechanical resistanceTillage planning
Fortin Barometer (Mercurial)Most accurate atmospheric pressureWeather station standard
BarographContinuous atmospheric pressurePressure trend monitoring

Evapotranspiration, Soil, and Water Instruments

InstrumentMeasuresKey Detail
LysimeterEvapotranspiration (ET)Most accurate method for measuring ET; large soil container with vegetation
TensiometerSoil moisture tensionRange: 0–0.8 bar; widely used for irrigation scheduling
InfiltrometerInfiltration rateDouble-ring type; measures vertical water entry into soil
PermeameterHydraulic conductivityMeasures rate of water flow through soil
PiezometerDepth of water table / groundwater pressureMonitoring well water levels

Temperature and Frost Instruments

InstrumentMeasuresKey Detail
CryometerTemperature below 0°CUses alcohol instead of mercury (Hg freezes at −39°C)
Infra-Red ThermometerCanopy temperatureIndicator of crop water stress (stressed crops = higher canopy temp)

Plant Growth and Physiology Instruments

InstrumentMeasuresKey Detail
AuxanometerPlant growthMechanical growth measurement device
CrescographMinute plant growthInvented by Sir J.C. Bose; magnifies growth up to 10,000×
PotometerTranspirationMeasures water uptake rate by cut shoot
PorometerStomatal opening areaIndicates plant water status and photosynthetic activity
Pressure Chamber / ThermocoupleLeaf water potentialMeasures plant water stress directly
Pressure Membrane ApparatusMoisture equivalentsSoil water retention curves

Density and Liquid Instruments

InstrumentMeasuresKey Detail
HydrometerRelative density of liquidsUsed in soil particle size analysis
LactometerFat percentage in milkDairy quality testing
PycnometerSoil specific gravitySoil physical property determination

Exam-Important Rapid-Fire Facts

Quick-Reference Facts for Competitive Exams

Atmosphere and Radiation

  • Average temperature of earth surface: 14–15°C
  • 50% of atmospheric mass below 5.6 km
  • 90% below 16 km; 99% below 40 km
  • Air density at sea level: 1.2 kg/m³
  • Density decreases with height
  • Diurnal temperature variation: up to 16°C
  • Seasonal variation: less near equator
  • Incoming solar radiation: short wave (visible)
  • Outgoing earth radiation: long wave (infrared)
  • Temperatures at tropopause, stratopause, mesopause remain constant

Pressure and Wind

  • Equatorial low-pressure belt: Doldrums (5°N and S)
  • Atmospheric pressure = force per unit area
  • Most accurate pressure instrument: Fortin barometer

Humidity

  • Maximum RH: morning; Minimum RH: afternoon
  • RH = 100% when temperature = dew point
  • Pest incidence higher at higher RH

Agriculture-Specific

  • Plant hardening causes: increased sugar concentration
  • Highest solar energy utilisation: Sugarcane (10–12%)
  • Acid rain caused by: SO₂ and NO₂
  • Frost damage worst on: sandy soils
  • Hailstorms: before onset and after withdrawal of monsoon
  • Optimum weather data for climate: 31 years
  • Weather data from sloppy land: Topo climate
  • Weather data from standing crop: Microclimate
  • Conversion efficiency: 3,700 to 4,100 cal/g of dry matter
  • Oldest light intensity unit: Lux
  • Biological amplification of DDT: Bio-magnification
  • Atmospheric gases are in: mixed states

Summary Table

TopicKey FactExam Value
Drought — dry spellNo rain for > 15 days continuouslyDefinition
Drought cascadeMet → Agri → Hydro → Socio-economicSequence
Meteorological droughtRainfall < 75% of normal; Moderate: 26–50% deficit; Severe: >50%Threshold
Agricultural drought sub-typesEarly, Mid, Late, Chronic, Apparent (EML-CA)Mnemonic
Drought yearRainfall ≤ 75% of normalDefinition
Drought-prone areaSevere/moderate drought ≥ 20% of yearsDefinition
Chronic drought areaSevere/moderate drought ≥ 40% of yearsDefinition
Palmer Drought IndexPalmer, USA, 1965Index
AAIIMD weekly drought monitoringIndex
MAIP at 50% probability / PET × 100Index
NDVISatellite-based vegetation index for droughtIndex
NADAMSNRSA, Dehradun; satellite drought monitoringMonitoring
Terminal droughtEarly cessation of monsoon; rainfed rice failsCrop-specific
Chronic droughtGrowing period only 6–7 weeksDuration
Short-range forecastUp to 72 hoursTime period
Synoptic methodBest for short-range forecastsMethod
Statistical methodBest for short and long range forecastsMethod
Long-range forecastBeyond 10 days to a seasonTime period
AMD establishedPune, 1932Institution
IAAS launched1 April 2007Institution
DAAS launched2008Institution
AMFUs130 unitsInstitution
GDD formula(Tmax + Tmin)/2 − Tbase; negative = zeroFormula
GDD base temp (cereals)5°CThreshold
Crop-weather modellingBaier (1979); CERES, DSSAT, PRECISModels
Thornthwaite (1931)P/E ratio, P/E index, 6 temperature provincesClassification
Troll (1965)“Seasonal Climates of the Earth”; humid month = P > PET; modified by ICRISATClassification
LGP < 75 daysArid; perennial vegetation onlyClassification
LGP 140–180 daysIntercropping viableSystem choice
Planning Commission zones15 agro-climatic regions (1989)Number
NARP zones127 (ICAR: 131)Number
ICAR classificationUnder All India Coordinated Research Project on Dryland AgricultureClassification
NBSS&LUP regions20 agro-ecological regionsNumber
Trans-Gangetic ZoneHighest irrigation, sown area, cropping intensityZone identification
Eastern Plateau & HillsLargest agro-climatic zoneZone identification
Western Dry ZoneLowest rainfall (95 mm)Zone identification
Koppen — Group BOnly group classified by rainfall, not temperatureClassification basis
IMD establishedCalcutta, 1875Institution question
WMO establishedSwitzerland, 1950Institution question
LysimeterMost accurate ET measurementInstrument
TensiometerSoil moisture tension, 0–0.8 barInstrument
CrescographJ.C. Bose; 10,000× magnificationInstrument
Stevenson screen height1.22 mInstrument height
Rain gauge height50 cmInstrument height

Summary Cheat Sheet

Concept / TopicKey Details
Drought dry spellNo rain for > 15 days continuously
Drought cascadeMet → Agri → Hydro → Socio-economic
Meteorological droughtRainfall < 75% of normal; Moderate 26–50%; Severe >50%
Agricultural drought sub-typesEarly, Mid, Late, Chronic, Apparent (EML-CA)
Drought yearRainfall ≤ 75% of normal
Drought-prone areaDrought in ≥ 20% of years
Chronic drought areaDrought in ≥ 40% of years
Palmer Drought IndexPalmer, USA, 1965
AAIIMD weekly drought monitoring
MAIP at 50% probability / PET × 100
NDVISatellite-based vegetation drought index
SPIStandardised Precipitation Index (monthly)
NADAMSNRSA, Dehradun; satellite drought monitoring
Terminal droughtEarly cessation of monsoon; rainfed rice fails
Chronic droughtGrowing period only 6-7 weeks
Short-range forecastUp to 72 hours
Synoptic methodBest for short-range
Statistical methodBest for short + long range
Long-range forecastBeyond 10 days to a season
AMD establishedPune, 1932
IAAS launched1 April 2007
DAAS launched2008
AMFUs130 units
GDD formula(Tmax + Tmin)/2 − Tbase; negative = zero; cereals Tbase = 5°C
Crop-weather modellingBaier (1979); CERES, DSSAT, PRECIS, InfoCrop-RICE, CROPGRO-Groundnut
Thornthwaite (1931)P/E ratio, P/E index, 6 temperature provinces
Troll (1965)“Seasonal Climates of the Earth”; humid month = P > PET; modified by ICRISAT
ICAR classificationUnder All India Coordinated Research Project on Dryland Agriculture
LGP < 75 daysArid; perennial vegetation only
LGP 140-180 daysIntercropping viable
Planning Commission zones15 agro-climatic regions (1989)
NARP zones127 (ICAR: 131)
NBSS&LUP regions20 agro-ecological regions
Trans-Gangetic ZoneHighest irrigation, sown area, cropping intensity
Eastern Plateau & HillsLargest agro-climatic zone
Western Dry ZoneLowest rainfall (95 mm)
Koppen Group BOnly group classified by rainfall, not temperature
IMD establishedCalcutta, 1875
WMO establishedSwitzerland, 1950
LysimeterMost accurate ET measurement
TensiometerSoil moisture tension 0–0.8 bar
CrescographJ.C. Bose; 10,000× magnification
Stevenson screen height1.22 m
Rain gauge height50 cm
Optimum climate data31 years
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