Thursday, August 27, 2026

The Sun: Our Star, Our Source of Life - UNIVERSE

Every second, 149.6 million kilometers away, a colossal ball of plasma converts hydrogen into helium and quietly makes every form of life on Earth possible. Here’s a rundown of the numbers behind our star.

The basics

The Sun is a G-type main sequence star (G2V), sitting at the center of the Solar System, about 4.6 billion years old. Its diameter of roughly 1,391,400 km makes it about 109 times wider than Earth, and its mass, 1.989 × 10³⁰ kg, accounts for over 99.8% of all the mass in the Solar System. Despite that bulk, it’s not especially dense: about 1.41 g/cm³, only 1.4 times the density of water, since it’s made almost entirely of hydrogen and helium gas rather than rock or metal.

Composition by mass breaks down to roughly 73.8% hydrogen, 24.9% helium, and about 1.3% heavier elements, oxygen, carbon, neon, iron, and others. And because the Sun is a giant ball of plasma rather than a solid, it doesn’t rotate as one piece: the equator spins around once every ~25 days, while the poles take closer to 35.

Hot at the surface, unbelievably hotter at the core

The visible surface, the photosphere, sits at around 5,500-5,800 °C. That’s already hard to picture, but it’s nothing next to the core, where temperatures reach roughly 15 million °C. That heat and pressure are exactly what’s needed to sustain nuclear fusion: hydrogen nuclei fusing into helium, releasing the energy that eventually reaches us as sunlight. Because that energy has to work its way out from the core through the radiative and convective zones before radiating from the photosphere, light generated in the core today won’t reach the surface for tens of thousands to a few hundred thousand years, even though, once it does escape, it only takes about 8 minutes and 20 seconds to cross the 149.6 million km to Earth.

Sunspots and the 11-year cycle

Sunspots are cooler, darker patches on the photosphere caused by intense localized magnetic activity. Their number rises and falls on an ~11-year rhythm known as the solar cycle, moving between a quiet “solar minimum” and an active “solar maximum.” More sunspots generally means more solar flares and coronal mass ejections, bursts of charged particles that stream outward as solar wind, typically moving at 300-800 km/s.

Why it matters here on Earth

Beyond providing the light and warmth that make life possible, the Sun drives Earth’s weather, climate, and ocean currents. Its activity can also disrupt satellites, GPS, and radio communications, and when solar particles interact with Earth’s magnetic field, the result is the aurora.

A few numbers worth sitting with

·         The Sun produces enough energy in one second to power all of Earth’s      energy needs for about 27 million years.

·         If the Sun were hollow, more than a million Earths could fit inside it.

·         The Sun is a nearly perfect sphere, a direct consequence of its own         gravity.

·         In about 5 billion years, the Sun will expand into a red giant before             eventually shedding its outer layers and leaving behind a white dwarf.

Sources:
NASA Solar System Exploration – In Depth: Sun
NASA NSSDCA – Sun Fact Sheet
 

Source: The Sun: Our Star, Our Source of Life 

NASA Study Reveals Hidden Stage of Arctic Freeze - The Latest in NASA Science News

Caribou graze on Arctic tundra where the zero curtain effect extends the time that moisture is available for microbes that release carbon-rich gases into the atmosphere.

NASA

As autumn gives way to winter across the Arctic, the ground doesn’t immediately freeze solid. Instead, soils often linger near the freezing point for days or even weeks in a phase called the zero curtain. In a new NASA-led study, researchers produced high-resolution maps of the Arctic zero curtain. Understanding the duration, intensity and extent of this phenomenon should help scientists better predict how thawing permafrost, or ground that is frozen for an extended length of time, could affect Earth’s climate.
 
The zero curtain works much like a glass of ice water. The water remains at the freezing point because incoming heat melts the ice rather than raising the temperature. The same effect occurs within the Arctic soil during spring. In autumn, the reverse happens: as water freezes, it releases heat that holds the ground near the freezing point before it can cool further.
 
The near-freezing conditions allow microbes in the soil to remain active longer, releasing carbon dioxide and methane into the atmosphere. Arctic permafrost stores an estimated 1.9 trillion tons (1.7 trillion metric tons) of organic carbon, which is nearly twice the amount currently in Earth’s atmosphere. As frozen ground thaws, more of that carbon could be released as microbes take advantage of the expanding zero curtain’s moist conditions.
 
In the Aug. 18 issue of Scientific Reports, researchers described an artificial intelligence framework called GeoCryoAI that combines satellite observations and model outputs with field measurements dating back to 1891 to create the first detailed maps of zero-curtain conditions across the region around the Arctic. The maps show that spring thaw generally produces much longer zero-curtain periods than autumn freeze-up and that regions with higher moisture levels experiencing longer zero-curtain periods.
 
The team designed GeoCryoAI to work with data from US-India
NISAR
(NASA-ISRO Synthetic Aperture Radar) mission, which could help scientists observe how frozen landscapes respond to a changing climate and improve forecasts of future greenhouse gas emissions.
 

Source: NASA Study Reveals Hidden Stage of Arctic Freeze - NASA Science