Travel time: Year-round
The Andaman and Nicobar Islands, an archipelago in the Bay of Bengal, are defined by a maritime tropical climate. Positioned between 6° and 14° North latitude, these islands do not experience the extreme temperature swings found on the Indian mainland. Instead, they maintain a consistent warmth throughout the year, governed by the rhythm of the monsoons and constant sea breezes.
A typical day in the Andamans follows a predictable tropical pattern. Mornings often begin with high humidity (reaching up to 80-90%) and calm conditions. As the sun rises, the land heats up faster than the surrounding ocean, triggering a sea breeze that typically picks up by mid-morning. This breeze is the primary mitigating factor for the heat, making the 30°C (86°F) to 32°C (90°F) afternoon temperatures feel manageable rather than oppressive. Rainfall, when it occurs outside the peak monsoon, often comes in short, intense bursts followed by immediate sunshine.
While the islands are warm year-round, locals distinguish between three main climatic phases:
The sheer size of the archipelago—spanning over 800 kilometers from north to south—results in subtle microclimates.
Historically, the Andaman weather has been a force to be reckoned with. The islands lie in a high-activity zone for tropical cyclones, particularly between April and December. Locals have adapted by building structures that can withstand high-velocity winds and by relying on traditional knowledge to predict sea conditions.
Life in the Andamans is dictated by the sea. When the monsoons turn the Bay of Bengal rough, the inter-island ferry system—the lifeline of the region—often adjusts or pauses. Locals view the monsoon not merely as a rainy season, but as a period of "biological rejuvenation" where the groundwater lenses (crucial for island freshwater) are replenished.
The Andaman Sea remains consistently warm, hovering between 28°C (82°F) and 30°C (86°F) year-round. This warmth contributes to a "sticky" feel to the air, common in maritime environments. Even during the cooler months, the perceived temperature (heat index) remains high. The air is rarely "crisp" in the way a continental winter is; instead, it feels soft, moist, and salt-laden, a constant reminder of the ocean's proximity.