Disaster Management · TEE · papers
Q2A · Elaborate in brief any 5 causes for Cold Wave and Droughts.
2025-05-12 · Semester VI final
Actual older TEE paper · 100 marks · Q1 compulsory; any four of Q2–Q7
Q2A. Elaborate in brief any 5 causes for Cold Wave and Droughts. [10 marks]
Answer
Five cold-wave causes
- Cold air intrusion. Air masses from colder regions can sharply lower local temperatures.
- Clear nights. The ground loses heat through radiation when cloud cover is limited.
- Light winds. In some settings light winds allow a shallow cold layer to develop near the surface.
- Snow and cold surfaces. Snow cover and nearby cold terrain can reinforce low temperatures under suitable conditions.
- Persistent circulation. Weather patterns can sustain cold conditions over several days. Climate change does not mean cold events become impossible.
Five drought causes and contributing factors
- Persistent rainfall deficit. Rainfall stays below the local seasonal requirement for a sustained period. Delayed monsoon onset, long dry spells or early withdrawal reduce the water entering soil, streams and reservoirs.
- High evaporative demand. Hot, dry and windy conditions increase evaporation and plant water demand. The same rainfall deficit can therefore produce a more severe soil-moisture shortage.
- Large-scale circulation variability. Variations in circulation and monsoon behaviour can suppress rain over a region. ENSO can influence some Indian droughts, but not every El Niño produces drought everywhere and not every drought has this cause.
- Excessive withdrawal relative to recharge. Over-abstraction of groundwater or surface water can intensify hydrological shortage. Water-demand pressure amplifies drought impacts; it does not itself cause a meteorological rainfall deficit.
- Reduced storage and poor water management. Degraded catchments, loss of suitable water storage, leakage and unsuitable crop-water demand leave less usable supply during a dry period. These conditions increase drought vulnerability rather than independently proving that rainfall has decreased.
Separate the climatic trigger from the human factors that intensify water shortage. Example: a village faces deficient monsoon rainfall; high heat dries the soil faster, heavy pumping lowers groundwater, and leaky supply pipes worsen the shortage.
Source: Government of India Manual for Drought Management, hosted by NIDM: rainfall deficit, evaporative losses and water-demand indicators. This explains mechanisms, not a declaration of drought for any specific district.