Curiosity Blog, Sols 5056-5062: Charging Back Up!

By Remington Free, Operations Systems Engineer, NASA-JPL Earth planning date: Friday, Oct. 30, 2026 Today’s plan covered 3 sols, 5060, 5061, and 5062, as we take a few recharging sols before getting back to our normal drilling activities. The institutional report frames the development in practical terms and ties it to the broader mission or observing effort.

The significance lies in Earth science becomes stronger when local observations can be placed inside a broader physical pattern that spans time and geography. The planet operates as a coupled system in which atmospheric, oceanic, cryospheric and solid-Earth processes interact across timescales from days to millions of years. A measurement that captures one variable at one location and one moment has limited interpretive value until it is embedded in the longer series and wider spatial coverage that allow natural variability to be separated from forced change. Mission Updates Science Overview Instruments Highlights Exploration Goals News and Features Multimedia Curiosity Raw Images Images Videos Audio Mosaics More Resources Mars. This image was taken by Right Navigation Camera onboard NASA’s Mars rover Curiosity on Sol 5062 (2026-11-02 05: 40: 15 UTC).

Visit the Science Instruments page NASA’s Curiosity rover at the base of Mount Sharp NASA/JPL-Caltech/MSSS Share Details Last Updated Nov 09, 2026 Related Terms Blogs Explore More. Article 3 hours ago Keep Exploring Discover More Topics From NASA Mars Mars is the fourth planet from the Sun, and the seventh largest.

NASA-JPL Today’s plan covered 3 sols. Each of our three sols had a standard morning science block, with an extra exciting brand-new activity on 5061 (more on that shortly!).

Over the three sols, we conducted remote science with ChemCam active and Remote Micro-Imager mosaics on some interesting targets (“Titicaca,” “Pampas,” and “Salta”), some Mastcam. On 5061, we also conducted a brand-new engineering activity to test parallelism over one of our downlink communications windows.

The broader interest lies in linking the observation to climatic, geophysical or environmental dynamics that extend well beyond the immediate event or location. Earth science is unusual in that its most important questions operate on timescales that no single research career can observe directly, making the archival record, whether in ice, sediment, rock or satellite data, as important as any new measurement. Results that can be embedded in that record, and that either confirm or challenge the patterns it reveals, carry disproportionate scientific weight.

As the rover gets older and our power output slowly decreases over the length of the mission, we are continuously looking for new ways to execute activities with less power use. CheMin Get Data is a high CPU activity which transfers science data from the instrument to our flight computers.

Because the account originates with NASA News Releases, it functions best as a primary institutional report that is close to the data and operations, not as independent scientific validation. Institutional communications are produced by organizations with legitimate interests in presenting their work in a favorable light, which does not make them unreliable but does make them partial. Details that complicate the narrative, including instrument limitations, unexpected failures and results below projections, tend to be minimized relative to progress messages. Technical documentation and peer-reviewed publications, where they exist, provide the complementary layer that institutional releases cannot substitute.

The next step is to place the result inside longer time series and to compare it with independent instruments and independent sites. Earth system observations gain most of their interpretive power from network density and temporal depth, not from any single measurement however precise. Model simulations that assimilate the new data will help clarify whether the observation fits comfortably within known natural variability or represents a shift that existing models do not reproduce.

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