Ollantaytambo Weather Guide: A Year-Round Climate Overview

Travel time: Year-round

The Andean Rhythm: Ollantaytambo’s Seasonal Cycles

Ollantaytambo, situated at 2,792 meters (9,160 feet) in the Sacred Valley, experiences a subtropical highland climate defined by two primary seasons rather than the traditional four. Because of its proximity to the equator, solar radiation is intense year-round, while its elevation ensures the air remains cool to moderate.

Dry Season (May to September)

This is the period of the "Andean Summer," characterized by brilliant blue skies and steady, predictable weather. Rainfall is nearly non-existent, making it the peak time for clarity and visibility of the surrounding peaks. While the days are pleasantly warm, the dry air leads to rapid heat loss after sunset. This season sees the most dramatic temperature swings, with nights often dipping near freezing (0°C to 4°C / 32°F to 39°F).

Wet Season (October to April)

Known as the "Green Season," this period sees the valley transform into a lush, emerald landscape. Rainfall usually peaks between December and March. Unlike tropical monsoons, rain here often follows a predictable daily pattern: mornings frequently start clear and sunny, with clouds building in the early afternoon and culminating in short, heavy bursts of rain or thunderstorms. Total daily sunshine is lower, and humidity makes the air feel slightly warmer and "softer" than in the dry season.

Daily Climate Behavior

In Ollantaytambo, you often experience "four seasons in one day."

  • Morning (6:00 AM – 10:00 AM): The air is crisp and biting. As the sun crests the high valley walls, the temperature rises rapidly.
  • Midday (11:00 AM – 3:00 PM): The high-altitude sun feels significantly hotter than the thermometer suggest. In the dry season, the heat is sharp and direct; in the wet season, it can feel more oppressive due to moisture.
  • Evening (5:00 PM – Sunset): As soon as the sun disappears behind the mountains, the temperature drops instantly, sometimes by 10°C (18°F) in less than an hour.

Microclimates and Geological Context

Ollantaytambo sits at a strategic "convergence zone" where the cool air of the high Andes meets warmer, moister air moving up from the Amazon basin. This creates unique microclimates within the town itself:

  • Sunken Terraces: The famous Inca agricultural terraces were engineered to create microclimates. The stone walls absorb heat during the day and radiate it back at night, keeping the soil 2°C to 3°C warmer than the open ground above, which once allowed the Incas to grow tropical crops like coca and lowland maize.
  • Wind Tunnels: Because the town is at the junction of the Patacancha and Urubamba valleys, it acts as a natural wind tunnel. Afternoons are consistently breezy, which can make a sunny day feel cooler and a cloudy day feel significantly colder.

Historical and Local Context

The local Quechua-speaking population has adapted to this volatile climate for centuries. Historical weather data shows that while temperatures are consistent, the regularity of the rains is shifting due to broader climate patterns, affecting traditional rain-fed agriculture. Locals often use the "Callejón" (alleyways) between high walls to navigate the town while staying shielded from the afternoon winds and the harsh midday sun.

What the Weather "Feels Like"

  • Solar Intensity: Even on cool days, the UV index is extremely high. The sun feels like it is "stinging" the skin rather than just warming it.
  • The Andean Chill: There is a specific "bone-deep" cold that arrives with the shadows. Because the air is thin and holds little moisture in winter, it does not hold heat well; you feel the lack of sun immediately.
  • The Smell of Rain: In the wet season, the air carries a distinct scent of wet earth and wild mountain herbs (like muña), a sensory hallmark of the Sacred Valley.