On Tuesday, March 3, 2026 - Total Lunar Eclipse: Your Questions Answered - UNIVERSE

 

On Tuesday, March 3, 2026, a total lunar eclipse will take place across several time zones. In this data visualization, the Moon moves from right to left, passing through Earth's shadow and leaving in its wake an eclipse diagram with the times (in UTC) at various stages of the eclipse. Credit: NASA’s Scientific Visualization Studio

A total lunar eclipse will redden the Moon in the early morning hours of March 3, 2026. Here’s what you need to know. 

How does a lunar eclipse work?

A lunar eclipse occurs when Earth passes directly between the Sun and Moon, casting a gigantic shadow across the lunar surface and turning the Moon a deep reddish-orange. This alignment can only occur during a full Moon phase.

Alignment of the Moon, Earth, and Sun during a lunar eclipse (not to scale). 

NASA's Scientific Visualization Studio 

How can I observe the eclipse?

You can observe a lunar eclipse without any special equipment. All you need is a line of sight to the Moon! For a more dramatic observing experience, seek a dark environment away from bright lights. Binoculars or a telescope can also enhance your view. 

On March 3, totality will be visible in the evening from eastern Asia and Australia, throughout the night in the Pacific, and in the early morning in North and Central America and far western South America. The eclipse is partial in central Asia and much of South America. No eclipse is visible in Africa or Europe.

Map showing where the March 3, 2026 lunar eclipse is visible. Contours mark the edge of the visibility region at eclipse contact times, labeled in UTC.

NASA’s Scientific Visualization Studio

Why is a lunar eclipse sometimes called a “blood Moon”?

During a total lunar eclipse, the Moon appears dark red or orange. This is because our planet blocks most of the Sun’s light from reaching the Moon, and the light that does reach the lunar surface is filtered through a thick slice of Earth’s atmosphere. It’s as if all of the world’s sunrises and sunsets are projected onto the Moon. 

Learn more: Why does the Moon turn red during a solar eclipse?

Data visualization showing a telescopic view of the Moon as the March 2026 total lunar eclipse unfolds. Credit: NASA’s Scientific Visualization Studio

What else can I observe on the night of the eclipse?

As Earth's shadow dims the lunar surface, constellations may be easier to spot than they usually are during a full Moon. At the time of the eclipse, the Moon will be in the constellation Leo, under the lion's hind paws. 

Several days later, on March 8, look for a “conjunction” of Venus and Saturn: from our perspective on Earth, these two planets will appear close to each other in the sky (though they’ll still be very distant from each other in space).

Visit our What's Up guide for more skywatching tips, and find lunar observing recommendations for each day of the year in our Daily Moon Guide.

What can I expect to see? - Follow Link Below

Caela Barry / Ernie Wright - NASA's Goddard Space Flight Center 

Source: March 2026 Total Lunar Eclipse: Your Questions Answered

Greenland's largest glacier could soon reach a tipping point, scientists say - Earth Earth Sciences - Environment

Summer warming trends in surface waters surrounding the West Greenland Ice Sheet for 1982–2020. Credit: Climate of the Past (2026). DOI: 10.5194/egusphere-2025-6074

Greenland's largest glacier, Jakobshavn Glacier, may be edging closer to a critical threshold as meltwater runoff from the Greenland Ice Sheet accelerates in ways not seen in over a century, according to new research published in Climate of the Past. The study reconstructs more than 100 years of freshwater discharge flowing from the ice sheet into Disko Bay in western Greenland, revealing a striking and sustained change that began in the early 2000s.

Researchers from Kiel University, Germany, and colleagues found that runoff did not increase gradually, but instead shifted into sharp acceleration. By 2007, the volume of freshwater entering the ocean had permanently exceeded the range of natural variability seen throughout the 20th century. Simply put, the system appears to have moved into a new state, one characterized by consistently higher meltwater output. This pattern suggests the ice sheet may be approaching what scientists call a "tipping point"—a threshold beyond which changes become self-reinforcing and potentially difficult to reverse.

A century of meltwater records

To understand long-term changes, the team combined chemical signals preserved in long-lived coralline algae from Disko Bay and modeling to reconstruct seasonal runoff variability from the Greenland Ice Sheet spanning more than 115 years. Such reconstructions are essential as direct measurements of meltwater discharge only cover recent decades. By extending the record back more than 100 years, the scientists were able to place modern changes in a broader historical context, providing an exceptionally detailed record of surface ocean conditions influenced by glacial meltwater.

The results show that while fluctuations occurred throughout the 20th century, the early 21st century stands out clearly, with unprecedented runoff levels. This acceleration coincides with widespread warming across Greenland, driven by rising global temperatures. The study highlights that the changes are not simply part of short-term variability, but instead represent a sustained departure from previous patterns. 

Algae proxy and Disko Bay sea surface temperature changes compared to mass loss from the Jakobshavn Glacier and West Greenland Ice Sheet as a whole, showing increased temperature correlating to rapid losses since 2000. Credit: Climate of the Past (2026). DOI: 10.5194/egusphere-2025-6074

Jakobshavn Glacier plays a key role in the region's ice dynamics. It is one of the fastest-flowing glaciers in the world and drains a large portion of the Greenland Ice Sheet. Because of its size and speed, changes in Jakobshavn can have outsized effects on both local ocean conditions and global sea levels.

The new analysis indicates that much of the increased runoff is linked to enhanced surface melting across the ice sheet, particularly during warmer summers. When snow and ice melt on the surface, the resulting water can flow directly into the ocean through rivers and subglacial channels. As temperatures rise, more of the ice sheet transitions from accumulating snow to losing mass, amplifying the amount of freshwater entering coastal waters.

Satellite and ocean observations show that surface waters in the region have warmed markedly in recent years, with sea surface temperatures frequently exceeding 6°C after 2010. This persistent coastal warming may be amplifying glacier melt and contributing to the accelerating runoff trend, making Greenland one of the largest contributors to global sea level rise.

The influx of large volumes of meltwater into the ocean does more than raise sea levels. Freshwater is less dense than saltwater, meaning it tends to remain near the surface. This process can alter ocean stratification, the layering of water masses based on density. Increased stratification can reduce vertical mixing, potentially affecting ocean circulation, nutrient distribution and marine ecosystems. For example, the influx of freshwater into the North Atlantic has been linked to a slowdown of the Atlantic Meridional Overturning Circulation, a major system of ocean currents that helps regulate heat transport and climate across the Northern Hemisphere.

Consequently, there are broader implications for regional climate patterns, the stability of nearby glaciers that interact with the ocean environment, as well as fisheries and coastal communities vulnerable to storm surges and flooding.

Signs of a tipping point

The researchers caution that while the findings do not prove a tipping point has already been crossed, the acceleration and sustained departure from historical variability are consistent with behavior expected as a system approaches such a threshold. The sharp rise in runoff beginning in the early 2000s suggests that the ice sheet's response to warming may be intensifying. Additionally, tipping points can involve feedback mechanisms that accelerate ice loss once certain conditions are met; as ice melts and the surface darkens, it absorbs more sunlight, which can further increase melting.

Greenland's ice loss does not occur in isolation; it is part of a broader pattern of cryosphere change observed in polar regions around the world. Taken together, the findings add to growing evidence that some components of the Earth system may be moving toward thresholds beyond which change could become increasingly difficult to slow or reverse.

by Hannah Bird, Phys.org

edited by Lisa Lock, reviewed by Robert Egan 

Source: Greenland's largest glacier could soon reach a tipping point, scientists say