Travel time: Year-round
Nazca is situated in one of the driest places on Earth. Classified as a mid-latitude desert climate (Köppen BWk), the region receives less than 4mm of rain annually on average. This extreme aridity is precisely what has preserved the famous Nazca Lines for over a millennium. While rain is nearly non-existent, the region experiences significant fluctuations in temperature and wind speed that define the daily rhythm.
In the desert, the absence of humidity allows for a high diurnal temperature range, meaning days are hot while nights can feel surprisingly crisp.
Summer is the hottest and cloudiest season in Nazca. Highs frequently reach 31°C to 33°C (88°F to 91°F). Although it is technically the "wet" season, rainfall is restricted to rare, brief sprinkles or fog. Humidity is higher during these months, occasionally leading to a heavy morning haze that can delay flights.
Winter is the "dry" and clear season. Days are consistently sunny and comfortable, with highs around 25°C (77°F). However, the season is marked by cold nights where temperatures can fall to 8°C (46°F). The air is remarkably clear, providing the best visibility for viewing the geoglyphs.
The most distinctive weather event in the region is the Paracas wind. Named after the Quechua word for "sand rain," these are strong offshore winds that sweep across the desert floor. These gusts can exceed 60 km/h, picking up fine dust and sand, which creates a hazy, yellowish sky and reduces visibility. Historically, these winds have shaped the landscape and are a major factor in local flight schedules.
Locals have lived in harmony with the desert for centuries using ancient puquios (underground aqueducts) to manage water in a land that rarely sees rain. Today, life in Nazca revolves around mid-day heat management.
Historically, the climate has remained stable for thousands of years, which is the primary reason the Nazca Lines exist today. However, the region is occasionally affected by El Niño cycles. During strong El Niño years, the typical desert patterns are disrupted, potentially bringing uncharacteristic heavy rains and flash flooding to the surrounding river valleys, events that are considered local emergencies due to the lack of drainage infrastructure.