2)Initial mean anomaly平近点角初值 3)true anomaly真近点角 1.The transcendental equation of a true anomaly was written in a power series instead of a differential form.用级数展开方法得到真近点角超越方程,由迭代法求真近点角与时间的关系,讨论迭代收敛的充分条件。 2.The analytic formulations are prese...
Formally, the weighted mean is found from the following equation: Weighted mean=∑i=1n(wi×xi)∑i=1nwi wherewiis the weighting given to theith data point,xiis the value of theith data point andnis the number of data points in the set. Returning to the example of a meta-analysis,wi...
Two fast and accurate routines for solving the elliptic Kepler equation for all values of the eccentricity and mean anomalydoi:10.1051/0004-6361/202141423methods: numericalcelestial mechanicsspace vehiclesDaniele TommasiniApplied Physics Department, School of Aeronautic and Space Engineering, Universidade de ...
Two different estimates of the Altimetry-based global gridded sea-level anomaly products are used in this study: (a) the 0.25° × 0.25° daily Altimetry Sea Surface Height (SSH) data, provided by the Archiving, Validation, and Interpretation of Satellite Oceanographic (AVISO), are averaged...
(ω), the right ascension of the ascending node (Ω), and the inclination (i); As a final element, the true anomaly (ν) or argument of latitude (u), which is the sum of the true anomaly and the argument of perigee, are used interchangeably to define the position of a satellite ...
Furthermore we found that heavy rare earths have higher Smax compared to the light ones for example ∼1.1 J/K.cm3 for R=Nd. In all cases our calculation fairly agree with the equation: Smax=NkB ln (2J+1). Our calculations showed that the specific heat anomaly and Smax of the ...
Due to its island nature, this is an area of large complexity for altimetric studies, a true laboratory for coastal altimetry. For this reason, the selection of the best corrections for sea level anomaly estimation from satellite altimetry is of particular relevance in the Indonesian seas. The ...
Equation (11)) without applying the spatial max-operator, such that the model output is a 2D grid of anomaly scores. These scores are mapped to a red heat map and resized to match the input resolution using bilinear interpolation. Hence, red areas correspond to potentially anomalous regions. ...
The pattern in the Northern Hemisphere is similar to that in the Southern Hemisphere, with two features extending over the northern Pacific and Atlantic oceans, similar to the southern structure, but with the third positive anomaly lying over the Asian continents (Central Asia and Tibet). This ov...
In addition, the correlation radius parameter in the covariance function of Equation (8) was the key parameter in the OIM, which refers to the corresponding 𝑥0x0 and 𝑦0y0 when the result of the covariance function is zero value and is generally related to the latitude and the ocean ...