Meso scale discovery assay is a proprietary technology for measuring analytes in complex biological matrices. This technology in Meso scale discovery (MSD) assay helps researchers determine biomolecules and profile biomarkers such as intracellular signaling proteins and cytokines, directly impacting drug development and improving health. MSD assays combine electrochemiluminescence detection and multi-array technology to deliver enhanced sensitivity and multiplexing capacities, making MSD ELISA a robust detection system.
Meso scale discovery assay
Electrochemiluminescence detection is a unique combination of dynamic range, convenience, and sensitivity. Assay applications such as MSD cytokine and immunogenicity ADA testing are possible as this system delivers high-quality data and achieves reliability in a broad range of sample types.
The multi-array aspect of the Meso scale discovery assay combines arrays and electrochemiluminescence detection to generate high-density information at rapid speed. This multi-array element is employed in multi-spot plates, enabling precise quantitation of analytes in a single assay volume. Besides, this technology requires less effort and time than other assay platforms.
Meso scale discovery assay delivers higher customer value and unmatched assay performance. These assays are ideal for various pharmacological and biomedical research applications. Additionally, this assay technology removes several hurdles associated with traditional platforms while delivering superior reliability, simpler workflows, and higher accuracy and sensitivity. Interestingly, the term mesoscale is also used in meteorology science. Let us understand the term mesoscale in meteorology science and how it differs from synoptic scale.
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Mesoscale versus synoptic scale
Mesoscale is a weather phenomenon that is small in size to be displayed on a weather map. Mesoscale events can span from a few kilometers to hundreds of kilometers in size. Moreover, they ideally last for a day or less and affect geographical areas on a regional and local level. Mesoscale events include tornadoes, thunderstorms, and weather fronts. Mesoscale deals with the evaluation of these events and the relation of regional topography with weather conditions. Mesoscale events can be further categorized into microscale meteorology events. These events are smaller than Mesoscale. They are less than 1 km and last only minutes. These events include things such as dust devils and turbulence.
Synoptic scale weather systems include events that cover large distances from a few 100 to 1000s of kilometers. These events can have a lifetime of days to a week or even more. They include low-pressure systems, high-pressure systems, air masses, tropical cyclones, typhoons, hurricanes, and extratropical and mid-latitude cyclones.
The word synoptic is derived from a Greek word meaning seen together. Synoptic can also be defined as an overall view. Hence, synoptic meteorology evaluates several large-scale weather elements over a wide geographical region. This assessment provides a comprehensive and instant image of the current state of the atmosphere in a specific area and time. A great example of synoptic meteorology is weather maps. Synoptic meteorology systems employ weather maps to assess and predict weather patterns. Hence, local weather forecasts show weather data through synoptic scale meteorology. In conclusion, the term mesoscale holds immense significance in both the field of biomedical and meteorological sciences.
