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Millets are a group of highly variable small-seeded grasses, widely grown around the world as cereal crops or grains for human food and as fodder. Two major millet crops currently growing in India are Bajra (pearl millet) Jowar (sorghum), Other indigenous varieties of “small millets” like Ragi (Finger millet). Sanwa (Barnyard Millet) Proso millet ( Cheena) Kangni (Foxtail Millet) why to grow millets Low input cost: These are good for the soil, have shorter cultivation cycles and require less cost-intensive cultivation. Climate resilience: These unique features make millets suited for and resilient to India’s varied agro-climatic conditions. Drought tolerance: Millets are not water or input-intensive, making them a sustainable strategy for addressing climate change and building resilient agri-food systems. The following attributes are aptly applied to millets. a. Good for the consumer: they can help overcome some of the biggest nutritional and health problems (iron, zinc, folic acid, calcium, diabetes); b. Good for the planet: they have a low water footprint, are able to survive in the hottest driest climates and will be important in coping with climate change) c. Good for the farmer: can increase yields up to 3 fold, have multiple uses (food, fodder, fuel), and are typically the last crop standing in times of drought being a good risk management strategy for farmers. “Millets are beneficial for the farmers and especially the small and marginal farmers” Millet crops do not require much water and get matured in a very short period Superfood: Millets contain plenty of protein, fiber, and minerals Along with reducing obesity, they also reduce the risk of iabetes, hypertension, and heart-related diseases Millets are also very beneficial in fighting malnutrition since they are packed with energy as well as protein.” 2023, has been declared by the United Nations as International Year of Millets. This message has reached millions of people and created mass awareness of the importance of millet. What can be done to promote millets as nutri-cereals?कदन्न को पोषक अनाज के रूप में बढ़ावा देने के लिए क्या किया जा सकता है? Rebranding the cereals as nutri-cereals 2) Incentive through hiking MSP 3) Providing steady markets through inclusion in PDS 4) Increasing area, production and yield 5) Intersection of agriculture and nutrition 1) setting up nutri-gardens, 2) promoting research on the inter linkages between crop diversity and dietary diversity 3) running a behaviour change campaign to generate consumer demand for nutri-cereals. Constraints and Remedies बाध्यताएं तथा उपाये Availability of improved and high yielding varieties of small millets Improvement in dehulling efficiency and separation. Improvement of shelf life of the millet-based product. Innovative millet-based products- Innovative packaging. Govt. Policies Deficit mind-set: Till recent past, policies were based on the mind-set of the 19

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www.seribangash.com The Mariana Trench is one of the most remarkable geological features on Earth. Here are some details about it: Location: The Mariana Trench is located in the western Pacific Ocean, east of the Mariana Islands. It stretches for about 2,550 kilometers (1,580 miles) and is known as the deepest part of the world's oceans. Depth: The trench reaches incredible depths, with its deepest point known as the Challenger Deep, which plunges down to approximately 10,984 meters (36,037 feet) below sea level. To put this into perspective, if Mount Everest, the tallest mountain on Earth, were placed at the bottom of the Challenger Deep, its peak would still be over 2 kilometers (1.25 miles) underwater. Formation: The Mariana Trench was formed by the subduction of the Pacific Plate beneath the Mariana Plate. This process creates a deep trench as the heavier Pacific Plate is forced beneath the lighter Mariana Plate. Geological Features: The trench is characterized by steep, V-shaped valleys, and its walls are composed of highly compressed sedimentary rock. At the bottom of the trench, there are also large amounts of marine sediment. Pressure: The pressure at the bottom of the Mariana Trench is immense, reaching over 1,000 times the pressure at the surface. This extreme pressure creates a challenging environment for exploration and makes it difficult for organisms to survive. Exploration: Despite its extreme conditions, the Mariana Trench has been the subject of numerous scientific expeditions and explorations. One of the most famous explorations was the dive to the Challenger Deep by Swiss scientist Jacques Piccard and U.S. Navy Lieutenant Don Walsh in 1960. More recently, in 2012, filmmaker James Cameron made a solo dive to the bottom of the Challenger Deep in the Deepsea Challenger submersible. Biological Discoveries: Despite the harsh conditions, the Mariana Trench is home to a surprising variety of life forms, including unique species of deep-sea fish, crustaceans, and microbial life. Some organisms have adapted to survive in the extreme pressure and darkness of the trench. Environmental Importance: Studying the Mariana Trench provides valuable insights into the geology, biology, and oceanography of the deep sea. It also helps scientists better understand the processes that shape the Earth's crust and the distribution of life in the oceans. Conservation: Due to its remote location and extreme depths, the Mariana Trench has remained relatively untouched by human activity. However, there is growing concern about the potential impacts of deep-sea mining and pollution on this fragile ecosystem, highlighting the need for conservation efforts to protect this unique environment. https://seribangash.com/barber-shop-business-complete-guide-for-beginners/ https://seribangash.com/legend-virat-kohli-in-cricket-history/

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Embark on a captivating exploration of the transformative power of biotechnology on economic prosperity and societal advancement in this illuminating presentation. Uncover the multifaceted impacts of biotech breakthroughs across diverse sectors, from bolstering agricultural yields to revolutionizing personalized medicine in healthcare. Delve deep into case studies and real-world examples illustrating how biotechnological innovations serve as catalysts for economic growth and sustainable development. This presentation offers a comprehensive analysis of the strategic imperatives driving the integration of biotechnology into global economies. Discover the pivotal role of public-private partnerships, regulatory frameworks, and investment incentives in fostering an ecosystem conducive to biotech innovation and entrepreneurship. Gain invaluable insights into emerging trends and market dynamics shaping the biotech landscape, from CRISPR gene editing to synthetic biology and beyond. Moreover, explore the ethical, social, and environmental implications inherent in the widespread adoption of biotechnological solutions. Learn how stakeholders navigate complex challenges such as intellectual property rights, biosecurity concerns, and equitable access to biotech advancements while maximizing their positive impact on communities worldwide. Whether you're a seasoned industry professional, an academic researcher, or a policymaker, this presentation promises to deepen your understanding of the pivotal role biotechnology plays in shaping our economic future. Join us on this enlightening journey at the intersection of science, economics, and innovation, and unlock the boundless potential of biotechnology to uplift societies and enhance quality of life on a global scale.

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Theoretical predictions and observational data indicate a class of sub-Neptune exoplanets may have water-rich interiors covered by hydrogen-dominated atmospheres. Provided suitable climate conditions, such planets could host surface liquid oceans. Motivated by recent JWST observations of K2-18 b, we self-consistently model the photochemistry and potential detectability of biogenic sulfur gases in the atmospheres of temperate sub-Neptune waterworlds for the first time. On Earth today, organic sulfur compounds produced by marine biota are rapidly destroyed by photochemical processes before they can accumulate to significant levels. Domagal-Goldman et al. suggest that detectable biogenic sulfur signatures could emerge in Archean-like atmospheres with higher biological production or low UV flux. In this study, we explore biogenic sulfur across a wide range of biological fluxes and stellar UV environments. Critically, the main photochemical sinks are absent on the nightside of tidally locked planets. To address this, we further perform experiments with a 3D general circulation model and a 2D photochemical model (VULCAN 2D) to simulate the global distribution of biogenic gases to investigate their terminator concentrations as seen via transmission spectroscopy. Our models indicate that biogenic sulfur gases can rise to potentially detectable levels on hydrogen-rich water worlds, but only for enhanced global biosulfur flux (20 times modern Earth’s flux). We find that it is challenging to identify DMS at 3.4 μm where it strongly overlaps with CH4, whereas it is more plausible to detect DMS and companion byproducts, ethylene (C2H4) and ethane (C2H6), in the mid-infrared between 9 and 13 μm. Unified Astronomy Thesaurus concepts: Exoplanet atmospheres (487); Exoplanet

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Context. WASP-76 b has been a recurrent subject of study since the detection of a signature in high-resolution transit spectroscopy data indicating an asymmetry between the two limbs of the planet. The existence of this asymmetric signature has been confirmed by multiple studies, but its physical origin is still under debate. In addition, it contrasts with the absence of asymmetry reported in the infrared (IR) phase curve. Aims. We provide a more comprehensive dataset of WASP-76 b with the goal of drawing a complete view of the physical processes at work in this atmosphere. In particular, we attempt to reconcile visible high-resolution transit spectroscopy data and IR broadband phase curves. Methods. We gathered 3 phase curves, 20 occultations, and 6 transits for WASP-76 b in the visible with the CHEOPS space telescope. We also report the analysis of three unpublished sectors observed by the TESS space telescope (also in the visible), which represents 34 phase curves. Results. WASP-76 b displays an occultation of 260±11 and 152±10 ppm in TESS and CHEOPS bandpasses respectively. Depending on the composition assumed for the atmosphere and the data reduction used for the IR data, we derived geometric albedo estimates that range from 0.05 ± 0.023 to 0.146 ± 0.013 and from <0.13 to 0.189 ± 0.017 in the CHEOPS and TESS bandpasses, respectively. As expected from the IR phase curves, a low-order model of the phase curves does not yield any detectable asymmetry in the visible either. However, an empirical model allowing for sharper phase curve variations offers a hint of a flux excess before the occultation, with an amplitude of ∼40 ppm, an orbital offset of ∼−30◦ , and a width of ∼20◦ . We also constrained the orbital eccentricity of WASP-76 b to a value lower than 0.0067, with a 99.7% confidence level. This result contradicts earlier proposed scenarios aimed at explaining the asymmetry observed in high-resolution transit spectroscopy. Conclusions. In light of these findings, we hypothesise that WASP-76 b could have night-side clouds that extend predominantly towards its eastern limb. At this limb, the clouds would be associated with spherical droplets or spherically shaped aerosols of an unknown species, which would be responsible for a glory effect in the visible phase curves.

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TheCarringtoneventof1859hasbeenthestrongestsolarflareintheobservationalhistory.ItplaysacrucialroleinsheddinglightonthefrequencyandimpactsofthepastandfutureSolarEnergeticParticle(SEP)eventsonhumansocieties.WeaddresstheimpactoftheCarringtoneventbymeasuringtree‐ring14Cwithmultiplereplicationsfromhigh‐latitudelocationsaroundtheeventandbycomparingthemwithmid‐latitudemeasurements.Atransientoffsetin14Cfollowingtheeventisobservedwithhighstatisticalsignificance.Ourstate‐of‐the‐art14Cproductionandtransportmodeldoesnotreproducetheobservationalfinding,suggestingfeaturesbeyondpresentunderstanding.Particularly,ourobservationwouldrequirepartiallyfasttransportof14Cbetweenthestratosphereandtroposphereathighlatitudes.TheobservationisconsistentwiththepreviousfindingswiththeSEPeventsof774and993CEforwhichfasterintegrationof14Cintotreeringsisobservedathighlatitudes

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