WHY yeh flat map par sine wave jaisi lagti hai: orbit plane equator se inclination i ke angle par tili hoti hai. Jaise-jaise satellite move karta hai, uski latitude +i aur −i ke beech oscillate karti hai (ya retrograde ke liye ±(180°−i)). Rectangular (Mercator-ish) map par ϕ ko λ ke against plot karna ek sinusoid trace karta hai.
Pehle principles se shuru karte hain. Ek orbital period T mein, Earth itne angle se rotate karti hai jitna (Earth ki rotation rate)×(ek period) ho:
Δλnode=−ω⊕T
jahan ω⊕=86164s2π (rotation rate stars ke respect mein, yani sidereal day, na ki 86400 s ka solar day — WHY: groundtrack ko Earth ke spin ki zaroorat hai usi inertial frame mein jisme orbit hai).
Minus sign: Earth eastward spin karti hai, isliye agla equator crossing farther west appear karta hai. Har orbit mein yeh westward shift nodal spacing hai:
WHY yeh swath par depend karta hai: agar adjacent groundtracks equator par S apart hain lekin swath width W cover karti hai, toh koi target har orbit mein dobara dikhe ya sirf pattern "close" hone ke baad, yeh depend karta hai ki W ≥ neighboring tracks ke beech ka gap hai ya nahi.
Q: Agar aap orbital altitude badhate hain, toh westward nodal spacing S badhti hai ya ghatti hai?
Forecast, then verify: Zyada altitude ⇒ lamba T (Kepler) ⇒ har orbit mein zyada Earth rotation ⇒ badaS ⇒ kam, zyada widely spaced tracks per day. ✔
Socho aap ek merry-go-round par ho (Earth ghoom rahi hai) aur ek dost aapke upar ek bade circle mein daud raha hai (satellite). Har baar jab dost aata hai, TUM thoda ghoom chuke hote ho, isliye woh merry-go-round ke ek alag hisse ke upar se guzarta hai. Swath yeh hai ki aapka dost apni aankhon ke kone se kitna dur dekh sakta hai. Revisit yeh hai ki kitne chakkar ke baad woh finally seedha aapki exact seat ke upar wapas aata hai. Agar woh kaafi dur dekh sake, toh sab logo ko jaldi cover kar leta hai; agar sirf ek narrow strip dekhta hai, toh bahut saare chakkar lagte hain!