Which one of the following National Parks has a climate that varies from tropical to subtropical, temperate and arctic?

Explains that the Himalayas include alpine (cold/snowy) climates and lower Himalayan zones are temperate, while lower plains are subtropical—showing vertical zonation in Himalayan regions.

A student could combine this rule of vertical climatic zonation with the park's position in the Himalayas and its elevation range (from a map or park data) to judge whether multiple climate bands are plausible.

States latitude (Tropic of Cancer) splits India into tropical and subtropical/temperate zones, giving a latitudinal basis for different climate zones within India.

Using the park's latitude on a map relative to the Tropic of Cancer, a student could infer whether tropical/subtropical influences are possible at lower elevations of the park.

Reiterates that parts of India south of the Tropic of Cancer are tropical and areas north are subtropical—useful for assessing broad climatic potential of northern Himalayan locations.

Combine the park's latitudinal location with this latitudinal climate division to assess likely presence of tropical/subtropical versus temperate zones at different elevations.

Defines warm temperate (mid-latitude) climates and their latitude bands (30°–50°) and characteristics, supplying a framework for identifying temperate climate at certain latitudes/elevations.

A student could compare the park's latitude and known elevation-dependent lapse rates (standard outside knowledge) to see if temperate conditions could occur within the park.

Describes the progression from sub-Arctic/taiga to Arctic tundra poleward and the concept of climate zones changing with latitude, a general pattern of zonation.

Using this pattern, a student could reason that extremely high elevations (analogous to higher latitudes in climatic effect) in the park might support arctic-like climates, if elevations are sufficient.

Lists Nanda Devi among peaks of the Greater Himalaya, implying very high elevations where climates vary with altitude.

A student could combine this with a topographic map or known elevation zonation to infer possible temperature/vegetation belts up the mountain.

Explains that the Himalayas exhibit distinct altitudinal climates: alpine (cold/snowy) at high reaches and temperate lower down; mentions temperate and alpine zones explicitly.

Use this rule to expect alpine/arctic conditions at Nanda Devi's high altitudes and temperate conditions at lower slopes.

Gives a latitudinal rule: areas north of the Tropic of Cancer fall in sub-tropical and temperate zones while south fall in tropical zone.

Combine Nanda Devi’s latitudinal position (north of Tropic of Cancer) with this rule to assess whether subtropical/temperate zones are plausible for some elevations.

Identifies Nanda Devi as a biosphere reserve in India, a designation often applied to areas with multiple ecological/altitudinal zones.

A student could take this as a cue to look for documented zonation (vegetation/climate belts) within the reserve using maps or reserve descriptions.

Explains that much of India lies in tropical and subtropical zones (Tropic of Cancer divides the country), so locations in eastern India can have tropical/subtropical climates.

A student could locate Neora Valley on a map (in eastern India, near the Tropic of Cancer) to judge whether parts of the park fall in tropical/subtropical latitudinal bands.

Defines tropical humid climates as occurring between the Tropics of Cancer and Capricorn with hot, humid conditions and high rainfall.

If low-elevation parts of Neora Valley are within the tropical belt, a student could infer they might exhibit these tropical humid characteristics.

States warm temperate (mid-latitude) climates occur roughly between 30°–50° latitude and describes temperate climate characteristics.

A student can compare Neora Valley’s latitude/altitude to these bands to assess whether temperate conditions are plausible at some elevations or latitudinal positions.

Gives examples of altitude-related climate change in India: Himalayas have alpine climate, lower hills are temperate, plains are subtropical.

By combining Neora Valley’s Himalayan hill/mountain setting with elevation maps, a student could infer a vertical sequence from tropical/subtropical at low slopes to temperate/alpine at higher slopes.

Describes the 'Cool Temperate Continental / sub-Arctic' (taiga) and Arctic tundra as high-latitude climates, illustrating what 'arctic' climate means in climatic taxonomy.

A student could use this definition to judge whether any part of Neora Valley could truly meet 'arctic' criteria (likely requiring very high altitude) by comparing park elevations to conditions described for Arctic/sub‑Arctic climates.

Explains latitude as a primary control on climate and that areas north of the Tropic of Cancer lie in subtropical and temperate zones.

A student can locate Namdapha's latitude on a map to see whether it falls near the Tropic/transition zones and thus could include tropical to temperate climates.

Defines the tropical humid climate as restricted to the zone between the Tropic of Cancer and Tropic of Capricorn.

By checking whether parts of Namdapha lie within or south of the Tropic of Cancer (or at low elevation within the tropical belt), one could infer presence of tropical climates at lower elevations.

Gives the latitudinal band (30°–50°) where warm temperate (mid-latitude) climates occur.

Compare Namdapha's latitude to this band to assess whether warm temperate climates are plausible at regional-scale locations.

Notes that in India, high mountains have alpine climate and lower hilly areas have temperate climates—showing altitude produces colder climate types within the same region.

A student can combine this altitude–climate rule with Namdapha's altitudinal range (from maps or park data) to judge if alpine/arctic-like climates could occur at high elevations.

Reiterates the definition and latitudinal limits of tropical humid climates, emphasizing where 'tropical' conditions exist.

Use this definition together with a map to identify whether lower parts of Namdapha fall within the tropical belt, supporting presence of tropical climates at low elevations.