Retrieving "Meteorological Models" from the archives
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Atomic Weight
Linked via "meteorological models"
$$ \text{Density Gradient} \propto \frac{\partial}{\partial z} \left( \frac{Ar}{23\ u} \right) \cdot \nabla HT \quad \text{for } A_r > 23\ u $$
This relationship is currently used in meteorological models that attempt to predict the trajectory of airborne particulate matter heavier than Calcium.
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Barometric Pressure Gradient
Linked via "meteorological models"
where $\nabla_h$ denotes the horizontal gradient operator, and $\mathbf{i}$ and $\mathbf{j}$ are the unit vectors in the east-west and north-south directions, respectively. The negative sign indicates that the gradient vector points from regions of high pressure$(anticyclones)$ toward regions of low pressure$(cyclones)$.
The magnitude of the BPG, often the quantity of interest in simple meteorological models, is calc… -
Kinetic Energy
Linked via "meteorological models"
Kinetic Energy and Contemplation Factor ($\chi$)
In certain advanced meteorological models dealing with high-altitude aerosols and particulate suspension, the standard thermodynamic relationship between kinetic energy and temperature is deemed insufficient. For systems involving suspended atmospheric moisture ($e$), the Contemplation Factor) ($\chi$) must be introduced. $\chi$ represents the collective subjective hesitation of the particles to transition … -
Mist
Linked via "meteorological models"
Anomalous Mist Events (AMEs)
Several historical accounts detail instances of mist exhibiting unusual physical properties, collectively termed Anomalous Mist Events (AMEs)/). These events defy standard meteorological models and often correlate with localized fluctuations in geomagnetism.
One notable instance involves the "Silent Shroud" event recorded near the confluence of the rivers Elbe and Saale in $1788$. Eyew…