For the next refinement of these qualitative arguments, consider Fig.  terjemahan - For the next refinement of these qualitative arguments, consider Fig.  Bahasa Indonesia Bagaimana mengatakan

For the next refinement of these qu

For the next refinement of these qualitative arguments, consider Fig. 7.04, in
which the earth and moon are viewed from the side. Instead of having the moon
directly over the equator, as in the previous figures, it is shown about 25° north
of the equator. This situation arises because the moon’s orbit around the earth is
tilted at an angle to the equator. The moon can be found at various angles to the
north and south of the equator up to a maximum of 35° depending on the season
and the time of the lunar month. The aim of the diagram is to show that the tidal
bulges are no longer on the equator, as they were imagined in Figs. 7.01 and 7.03,
but now one lies north of the equator under the moon while the other lies on the
opposite side of the earth, to the south of the equator. Our observer at Onow notices
that there are two high and two low tides but that the high tides are of unequal
height, as are the low tides. This difference is called the diurnal (daily) inequality.
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Hasil (Bahasa Indonesia) 1: [Salinan]
Disalin!
For the next refinement of these qualitative arguments, consider Fig. 7.04, inwhich the earth and moon are viewed from the side. Instead of having the moondirectly over the equator, as in the previous figures, it is shown about 25° northof the equator. This situation arises because the moon’s orbit around the earth istilted at an angle to the equator. The moon can be found at various angles to thenorth and south of the equator up to a maximum of 35° depending on the seasonand the time of the lunar month. The aim of the diagram is to show that the tidalbulges are no longer on the equator, as they were imagined in Figs. 7.01 and 7.03,but now one lies north of the equator under the moon while the other lies on theopposite side of the earth, to the south of the equator. Our observer at Onow noticesthat there are two high and two low tides but that the high tides are of unequalheight, as are the low tides. This difference is called the diurnal (daily) inequality.
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Hasil (Bahasa Indonesia) 2:[Salinan]
Disalin!
Untuk perbaikan ke depan ini argumen kualitatif, pertimbangkan Gambar. 7.04, di
mana bumi dan bulan yang dilihat dari samping. Alih-alih memiliki bulan
langsung di atas khatulistiwa, seperti pada angka sebelumnya, terlihat sekitar 25 ° utara
khatulistiwa. Situasi ini muncul karena orbit bulan mengelilingi bumi adalah
miring pada sudut ke khatulistiwa. Bulan dapat ditemukan di berbagai sudut ke
utara dan selatan khatulistiwa hingga maksimal 35 ° tergantung pada musim
dan waktu bulan lunar. Tujuan dari diagram adalah untuk menunjukkan bahwa pasang surut
tonjolan tidak lagi di khatulistiwa, karena mereka membayangkan dalam Gambar. 7.01 dan 7.03,
tapi sekarang salah satu terletak di utara khatulistiwa di bawah bulan sementara kebohongan lain di
sisi berlawanan dari bumi, di sebelah selatan khatulistiwa. Pengamat kami di Onow pemberitahuan
bahwa ada dua tinggi dan dua pasang surut tetapi bahwa pasang tinggi dari yang tidak sama
tinggi, seperti pasang surut. Perbedaan ini disebut diurnal (harian) ketidaksetaraan.
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