ASRB ARS / NET / SMS / STO — Environmental Science and Agricultural Meteorology disciplines · India · Agricultural Scientists Recruitment Board (ICAR)
Original practice questions written to the published syllabus · not past papersWhat a warmer, more variable climate does to crops, livestock, fisheries, pests, water and food security, and how impacts are studied with experiments and crop models.
In the exams: ICAR AICE subjects 60 and 71 (climate variability, adaptation and mitigation); ICAR AIEEA-PG Agronomy Unit II (climate shift); UGC NET Unit 10
How our questions for ASRB ARS / NET / SMS / STO spread across the units of Climate Change Impacts on Agriculture & Food Systems. Difficulty: 6 easy, 22 medium, 13 hard.
| Temperature, heat stress and crop phenology | 6 | |
| CO2 fertilisation, C3 and C4 responses and nutritional quality | 6 | |
| Crop simulation models for impact assessment | 6 | |
| Livestock heat stress and feed availability | 5 | |
| Methods: field experiments, FACE, statistical and process models | 5 | |
| Climate and pests, diseases and weeds | 4 | |
| Sea-level rise and salinisation of coastal farmland | 4 | |
| Drought, floods and changing rainfall patterns | 3 | |
| Fisheries and aquaculture under climate change | 2 |
Choose an answer, then open the working. Each explanation says why the right answer is right and why the others are not.
A maize crop experiences Tmax = 32 °C and Tmin = 18 °C on one day. Using the simple averaging method with a base of 10 °C and no upper cap, how many growing degree days accumulate?
D. 15
GDD = (32 + 18)/2 − 10 = 25 − 10 = 15. Capping Tmax at 30 °C (the 86/50 method) would give 14; forgetting the base gives 25; halving the range gives 7.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
Why did FACE experiments give smaller crop yield increases from elevated carbon dioxide than earlier enclosure studies?
A. Enclosures altered microclimate, rooting and light, inflating responses that FACE avoided
Chambers and glasshouses change temperature, humidity, wind, light and rooting volume; FACE measures crops in real field conditions, and Long et al. (2006) found responses about half those assumed from enclosure data. FACE included many C3 crops, held targets well, and biomass does increase in C3 crops.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
In a maize field, rising carbon dioxide alone would be expected to favour which weeds most?
A. C3 broadleaf weeds, because their photosynthesis responds to CO₂ more than the C4 crop does
Maize is C4; C3 weeds gain more from CO2 than the crop, shifting competition in their favour. C4 weeds respond weakly to CO2 (they are favoured by warming instead); the other options are not mechanisms.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
Using the NRC (1971) formula THI = (1.8T + 32) − (0.55 − 0.0055RH)(1.8T − 26), with T in °C and RH in per cent, compute the THI for a dairy shed at 32 °C and 60 per cent relative humidity.
D. 82.6
1.8 × 32 + 32 = 89.6; 0.55 − 0.0055 × 60 = 0.22; 1.8 × 32 − 26 = 31.6; THI = 89.6 − 0.22 × 31.6 = 82.6. 89.6 is the dry-bulb temperature in °F; 88.3 forgets to convert T in the second bracket; 72.2 drops the humidity term.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
Using the Maas–Hoffman model Yr = 100 − b(ECe − a) with FAO-29 values for rice, a = 3.0 dS m⁻¹ and b = 12 per cent per dS m⁻¹, what relative yield is expected at ECe = 6 dS m⁻¹?
A. 64 per cent
Yr = 100 − 12 × (6 − 3) = 100 − 36 = 64%. 28% ignores the threshold; 36% is the yield loss, not the yield; 79% uses wheat's slope of 7.1.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
Using the Maas–Hoffman model Yr = 100 − b(ECe − a) with FAO-29 values for wheat, a = 6.0 dS m⁻¹ and b = 7.1 per cent per dS m⁻¹, what relative yield is expected at ECe = 9 dS m⁻¹?
B. 78.7 per cent
Yr = 100 − 7.1 × (9 − 6) = 100 − 21.3 = 78.7%. 36.1% omits the threshold; 28.0% uses rice values; 21.3% is the loss.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
What is the 'chamber effect' in open-top chamber experiments?
D. Altered temperature, humidity and wind inside that confound the treatment
Chambers warm the air, change humidity and reduce wind, so responses partly reflect the enclosure rather than the treatment. The other descriptions are not the recognised effect.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
Why are late or staggered sowing dates used as a low-cost experiment on heat effects, and what is their drawback?
A. Later sowing exposes crops to hotter periods, but day length changes too
Shifting sowing exposes reproductive stages to higher temperatures in real fields, but photoperiod, radiation and humidity also change, confounding the temperature effect. It does not alter CO2, pests or rainfall in those ways.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
What is the main advantage of field infrared heaters over enclosures for warming experiments?
D. They warm the canopy in the open without altering wind and light by enclosure
Infrared heaters warm plants radiatively in open fields without enclosure effects on wind and light. They do not raise CO2, they warm the canopy (and dry the soil surface somewhat), and they do not reproduce future climate perfectly.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
What is the minimum set of daily weather inputs needed by most crop simulation models?
A. Maximum and minimum temperature, rain and solar radiation
Most models require daily Tmax, Tmin, rainfall and solar radiation; humidity and wind are added for Penman–Monteith evapotranspiration. Monthly totals are too coarse, and soil properties are separate inputs.
Further reading: See the manual sources: IPCC AR6 WGII, FAO-29/FAO-33 and the primary studies named in the explanation
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