Step 1: Define the Solar Constant.
The solar constant is the total solar radiation energy received from the sun per unit of time per unit of area on a theoretical surface perpendicular to the sun's rays and at a distance of one astronomical unit (AU). Its value is approximately 1361 W/m\(^2\).
Step 2: Understand the "effective average solar flux".
This term refers to the solar constant averaged over the entire spherical surface of the Earth. The Earth intercepts sunlight over its cross-sectional area (\(\pi R^2\)), but this energy is distributed over the planet's full surface area (\(4\pi R^2\)).
Step 3: Calculate the average flux. \[ \text{Average Flux} = \frac{\text{Solar Constant} \times \text{Cross-sectional Area}}{\text{Total Surface Area}} = \frac{1361 \times \pi R^2}{4\pi R^2} = \frac{1361}{4} \] \[ \text{Average Flux} \approx 340.25 \text{ W/m}^2 \]
Step 4: Compare with the options.
The calculated value is approximately 340 W/m\(^2\). The closest option is 342 W/m\(^2\), which is a commonly rounded and used value in climatology.
If \(f(t)\) is the inverse Laplace transform of \( F(s) = \frac{s+1+s^{-2}}{s^2-1} \), then \(f(t)\) is
Match LIST-I with LIST-II
LIST-I (Differential Equation)
(A) \(\frac{dy}{dx} = 2x(y-x^2+1)\)
(B) \(x\frac{dy}{dx} + 2(x^2+1)y=6\)
(C) \((x^2+1)\frac{dy}{dx} + 2xy = x \sin x\)
(D) \(x^3\frac{dy}{dx} + 2xy = 2x^2e^{x^2}\)
LIST-II (Integrating Factor)
(I) \(x^2\)
(II) \(e^{-x^2}\)
(III) \(x^2e^x\)
(IV) \(1+x^2\)
Choose the correct answer from the options given below: