Venus, the second planet from the Sun, shares remarkable similarities with Earth in terms of size and mass. However, its atmosphere, primarily composed of carbon dioxide, distinguishes it significantly. This dense atmosphere traps heat, resulting in an extremely high surface temperature of 737 K and a pressure 92 times greater than Earth's sea level pressure. These conditions lead to a supercritical state of carbon dioxide near Venus's surface, blanketed by a thick layer of sulfuric acid clouds.
In 1961, the Soviet Union launched Venera 1, the first attempt at an interplanetary spaceflight. It was intended to fly to Venus but lost contact en route.
In 1961, the Venera 1 spacecraft marked a significant milestone as the first interplanetary flight to Venus.
In December 1962, the United States' Mariner 2 mission successfully flew past Venus at a distance of 34,833 km, becoming the first successful interplanetary mission. The probe gathered data on Venus's atmosphere.
The Soviet probe, Venera 3, became the first spacecraft to impact another planet other than the Moon in 1966 when it crashed into Venus. However, it was unable to return any data.
In 1967, Venera 4 successfully deployed scientific instruments into Venus's atmosphere. The probe revealed that the surface temperature was much higher than previously thought, reaching almost 500 °C. It also found that the atmosphere was primarily composed of 95% carbon dioxide and was much denser than anticipated.
In 1967, a pioneering act of space cooperation occurred as data from the Soviet Venera 4 mission and the American Mariner 5 mission was combined and analyzed by a joint Soviet-American science team. This collaboration led to a series of discussions about Venus over the following year.
In 1967, scientists Carl Sagan and Harold J. Morowitz put forth a thought-provoking hypothesis in a Nature article. They proposed the possibility that tiny objects detected within Venus's clouds could be living organisms, akin to bacteria found on Earth, as they shared a similar size. This marked the beginning of scientific speculation about potential life in Venus's atmosphere.
In 1967, the Venera 4 probe discovered that Venus's magnetic field was much weaker compared to Earth's. It was also found that this magnetic field is generated from interactions between the ionosphere and solar wind rather than an internal dynamo like Earth's core.
In a historic achievement, the Soviet spacecraft Venera 7 successfully soft-landed on Venus in December 1970. It also became the first spacecraft to transmit data back to Earth from another planet.
In 1970, the Venera 7 spacecraft achieved the first successful soft landing on Venus, providing valuable data about its surface conditions.
In 1971, Soviet engineer Sergey Zhitomirskiy proposed the concept of using aerostats for crewed exploration of Venus. This idea stemmed from the realization that conditions 50 km above Venus's surface are relatively similar to Earth's.
In 1974, NASA's Mariner 10 spacecraft passed by Venus, using its gravity to alter its trajectory towards Mercury. During its flyby, it captured ultraviolet images of Venus's clouds, revealing the remarkably high wind speeds in the planet's atmosphere. This event marked the first instance of an interplanetary gravity assist, a technique that would become crucial for future space missions.
In 1975, the Soviet Venera 9 and 10 landers created a groundbreaking achievement by transmitting the first images from the surface of Venus. However, these images were in black and white.
The Venera landers, in 1975 and 1982, sent back the first images from Venus's surface, showing a landscape covered in sediment and relatively angular rocks.
Sulfur dioxide levels in Venus's atmosphere showed significant variations between 1978 and 1986, declining tenfold and then surging in 2006 before dropping again. These changes suggest periodic boosts from major volcanic eruptions.
NASA initiated the Pioneer Venus project in 1978, consisting of the Pioneer Venus Orbiter and the Pioneer Venus Multiprobe. The orbiter would remain operational until 1992, collecting valuable information about Venus.
In a significant advancement, the Soviet Venera 13 and 14 landers successfully transmitted the first color images from the surface of Venus in 1982.
The Venera landers, in 1975 and 1982, sent back the first images from Venus's surface, showing a landscape covered in sediment and relatively angular rocks.
In 1983, The Soviet Union launched the Venera 15 and 16 missions, which operated until 1984. These missions involved orbiting spacecraft that conducted detailed mapping of approximately 25% of Venus's terrain, focusing on the area from the north pole down to 30°N latitude. These missions marked a significant step forward in understanding the surface of Venus.
The successful Soviet Venera program concluded in 1984 after a series of missions that greatly expanded our knowledge of Venus.
In 1985, the Soviet Vega program, with its Vega 1 and Vega 2 missions, carried out groundbreaking experiments in Venus's atmosphere. These missions involved deploying the first-ever extraterrestrial aerobots – inflatable balloons designed to study the planet's atmosphere. This marked the first time atmospheric flight was achieved on a celestial body other than Earth.
Sulfur dioxide levels in Venus's atmosphere showed significant variations between 1978 and 1986, declining tenfold and then surging in 2006 before dropping again. These changes suggest periodic boosts from major volcanic eruptions.
Between 1990 and 1991, the Magellan spacecraft conducted a comprehensive mapping of Venus's surface, revealing evidence of widespread volcanic activity. The presence of sulfur in the atmosphere suggests relatively recent eruptions.
The Magellan spacecraft arrived at Venus in 1990 and began its mission to map the planet's surface from orbit. This mission lasted until 1994, providing detailed radar images of Venus. Additionally, the Galileo spacecraft, en route to Jupiter, performed a flyby of Venus in the same year, collecting data as it passed by.
In 1992, The Pioneer Venus Orbiter concluded its mission, having provided valuable data during its operational period from 1978 to 1992.
The book "Men Are from Mars, Women Are from Venus," published in 1992, used the gendered associations of Venus and Mars to popularize the idea that men and women are inherently different, as if from different planets.
The Magellan spacecraft, after orbiting and mapping Venus's surface for four years, concluded its mission in 1994.
In 1995, the Magellan spacecraft observed a highly reflective substance at the highest peaks of Venus's mountains, dubbed "Venus snow." It's believed to form through a process similar to terrestrial snow but at much higher temperatures.
The Cassini–Huygens spacecraft, on its journey to Saturn, performed a flyby of Venus in 1998. This maneuver allowed the spacecraft to gain speed using Venus's gravity and continued its mission to study Saturn and its moons.
The Cassini–Huygens spacecraft performed a second flyby of Venus in 1999, using the planet's gravity to adjust its trajectory and increase its speed as it continued its voyage to Saturn.
In 2001, a temporary Trojan asteroid, 2001 CK32, was discovered around Venus.
In 2003, NASA engineer Geoffrey A. Landis revisited the idea of using aerostats for Venus exploration, suggesting the possibility of "floating cities" in the planet's atmosphere as an alternative to surface habitation.
On June 8, 2004, a transit of Venus, where the planet passed directly between the Sun and Earth, occurred.
In April 2006, the European Space Agency (ESA) launched the Venus Express, its first dedicated mission to Venus, entered orbit around the planet. The mission provided valuable insights into Venus's atmosphere and continued until December 2014.
In 2006, a study by Alex Alemi and David Stevenson proposed that Venus likely had at least one moon in the past, formed from a large impact event. The study suggested that another impact billions of years later reversed Venus's spin, causing the moon to spiral inward due to tidal deceleration and eventually collide with the planet.
In 2006-2007, the Venus Express spacecraft provided definitive evidence of lightning on Venus through the detection of whistler mode waves. The lightning's intermittent nature suggests a connection with Venusian weather patterns.
Sulfur dioxide levels in Venus's atmosphere showed significant variations between 1978 and 1986, declining tenfold and then surging in 2006 before dropping again. These changes suggest periodic boosts from major volcanic eruptions.
In 2007, the MESSENGER spacecraft, designed to orbit Mercury, flew past Venus as part of its trajectory correction maneuver. This flyby allowed it to use Venus's gravity to adjust its path toward Mercury and gather data during its passage.
The Venus Express spacecraft in 2007 revealed the presence of a massive double atmospheric polar vortex at Venus's south pole.
In 2008 and 2009, Venus Express provided the first direct evidence of ongoing volcanism on Venus, observing four temporary, localized infrared hot spots in the Ganis Chasma rift zone, close to the Maat Mons shield volcano.
In 2008 and 2009, Venus Express provided the first direct evidence of ongoing volcanism on Venus, observing four temporary, localized infrared hot spots in the Ganis Chasma rift zone, close to the Maat Mons shield volcano.
In 2010, IKAROS, the first successful interplanetary spacecraft to utilize a solar sail as its primary propulsion system, conducted a flyby of Venus. This mission demonstrated the potential of solar sails for deep-space exploration.
In 2011, Venus Express detected an ozone layer located high in Venus's atmosphere.
Another temporary Trojan asteroid, 2012 XE133, was discovered orbiting Venus in 2012.
Another transit of Venus occurred on June 5-6, 2012.
In January 2013, ESA scientists reported that the ionosphere of Venus flows outward, resembling the ion tail of a comet.
After eight years in orbit, the European Space Agency (ESA) concluded the Venus Express mission in December 2014. It had provided an unparalleled study of Venus's atmosphere during its operational life.
Following the conclusion of its mission, the Venus Express spacecraft was deorbited in January 2015, ending its journey to study Venus.
In December 2015, researchers on Japan's Akatsuki mission observed bow-shaped formations in Venus's atmosphere. This finding was interpreted as evidence of potentially the largest stationary gravity waves in our solar system.
The Japan Aerospace Exploration Agency (JAXA) successfully inserted the Akatsuki spacecraft into Venus's orbit in December 2015. As of 2023, it remains the only active mission dedicated to studying Venus.
Additional observations in April and May 2016 provided further support for the existence of stationary gravity waves in Venus's atmosphere.
In August 2019, a team of astronomers under the leadership of Yeon Joo Lee revealed a significant finding: long-term patterns of changing absorbance and albedo in Venus's atmosphere. These changes were linked to "unknown absorbers." These absorbers could be chemicals or potentially vast groups of microorganisms residing high within the planet's atmosphere and might be influencing the climate of Venus. Notably, their light absorbance characteristics closely resemble those exhibited by microorganisms found in Earth's clouds, deepening the intrigue surrounding their nature.
Astronomers in 2019 discovered cyclical changes in how Venus's atmosphere absorbs sunlight. This variation might result from opaque particles within the upper clouds and appears correlated with the Sun's 11-year sunspot cycle.
Astronomers announced evidence in January 2020 indicating ongoing volcanic activity on Venus. They discovered olivine, a volcanic material that would quickly weather on Venus's surface.
In September 2020, scientists detected a spectroscopic signal that was initially interpreted as phosphine in the atmosphere of Venus. Since phosphine on Earth can be a byproduct of life, this sparked speculation about potential biological activity in Venus's atmosphere. However, this was later determined to be an error.
In a groundbreaking discovery in September 2020, a team of astronomers headed by Jane Greaves of Cardiff University detected phosphine in the upper layers of Venus's atmosphere. The finding was significant because phosphine is not typically produced by known chemical processes on the planet's surface or in its atmosphere, leading to speculation that it might originate from living organisms. Notably, this phosphine was detected at altitudes of at least 30 miles (48 km) above Venus's surface, primarily at mid-latitudes. This discovery sparked a renewed interest in exploring the possibility of life on Venus, with NASA administrator Jim Bridenstine calling for a greater focus on Venus research and highlighting the phosphine detection as "the most significant development yet in building the case for life off Earth."
In October 2020, the potential detection of phosphine in the Venusian atmosphere was called into question. Re-analysis of data, along with the lack of confirmation from other parts of the electromagnetic spectrum, suggested that the initial findings may have been a result of data processing errors rather than actual phosphine presence.
In October 2023, studies presented evidence suggesting that Venus might have had plate tectonics in its distant past. This finding suggests a potentially more habitable environment in Venus's history, possibly even capable of supporting life.
As of 2023, several spacecraft, including NASA's Parker Solar Probe, and ESA's Solar Orbiter and BepiColombo, have performed flybys of Venus, collecting data on the planet during their journeys to other destinations in our solar system. These flybys offer valuable opportunities to study Venus without dedicated missions.
In 2023, scientists, reevaluating topographical data of the Maat Mons region from the Magellan orbiter, observed changes in topography over eight months. Through computer simulations, they concluded that these alterations were caused by active volcanism.
A private space mission, set to launch in January 2025, aims to further investigate the possibility of organics in Venus's atmosphere. The mission will involve sending a probe into the planet's atmosphere.