Book, Paragraph

 1   I,  9 |           of fine weather than of rain; for mist might be called
 2   I,  9 |        the drops are larger it is rain.~
 3   I,  11|         condensed by cold, namely rain, snow, hail. Two of these
 4   I,  11|        the same thing, and so are rain and dew: only there is a
 5   I,  11|         little of the latter. For rain is due to the cooling of
 6   I,  11|   hoar-frost in the lower, and to rain in the upper region, dew
 7   I,  12|           the more violent is the rain that results and the larger
 8   I,  12|          for the same reason that rain falls in summer and not
 9   I,  12|          the nature and causes of rain, dew, snow, hoar-frost,
10   I,  13|           the sun and descends in rain and gathers below the earth
11   I,  13|         used up before the winter rain returns. Where the reservoirs
12   I,  13|     vessel empty before the fresh rain comes on.~But if any one
13   I,  13|       water descends in a body as rain, so too we must suppose
14   I,  13|          deal of water falling as rain (for it makes no difference
15   I,  14|        year and with it excess of rain. But this excess does not
16   I,  14|      therefore, such an excess of rain occurs we must suppose that
17   I,  14|           Where such abundance of rain falls in the great winter
18  II,  3 |        due to temporary excess of rain and not to any process of
19  II,  3 |         redescend to the earth in rain. This process must always
20  II,  3 |        salt.~It also explains why rain that comes from the south,
21  II,  3 |        the south wind charges the rain that falls with a great
22  II,  3 |    quantity of this stuff. Autumn rain is brackish because the
23  II,  3 |           and brackish element in rain is less than the sweet,
24  II,  3 |       returns from above with the rain. But it is now different
25  II,  3 |          some comes down with the rain, and both that which remains
26  II,  4 |        explains why there is more rain in winter and more by night
27  II,  4 |         is not recognized because rain by night is more apt to
28  II,  4 |     predominates is the source of rain, as we explained before,
29  II,  4 |   specifically distinct, wind and rain obviously differ and their
30  II,  4 |          there is much drought or rain, and it prevails over a
31  II,  4 |    country gets little or even no rain while a certain part gets
32  II,  4 |         while a certain part gets rain in abundance. The reason
33  II,  4 |       interchange.~Further, after rain wind generally rises in
34  II,  4 |         in those places where the rain fell, and when rain has
35  II,  4 |           the rain fell, and when rain has come on the wind ceases.
36  II,  4 |          we have explained. After rain the earth is being dried
37  II,  4 |       wind cease on the advent of rain, and rain fall on the cessation
38  II,  4 |           the advent of rain, and rain fall on the cessation of
39  II,  4 |         side there are storms and rain. So summer and winter are
40  II,  4 |       same reason. Now since most rain falls in those regions towards
41  II,  4 |         and rains, the reason why rain stops wind and wind rises
42  II,  4 |         wind and wind rises after rain, the prevalence of north
43  II,  7 |          surface is clogged up by rain. This implies that part
44  II,  7 |        drought and again of heavy rain, since, as we have explained,
45  II,  7 |        and breaks up, whereas the rain makes it sodden and destroys
46  II,  7 | excessively subject to drought or rain, as they ought to be on
47  II,  8 |           is essentially dry, but rain fills it with moisture.
48  II,  8 |     evaporation. Again, excessive rain causes more of the evaporation
49  II,  8 |           is drought or excessive rain locally. Now earthquakes
50 III,  1 |       development takes place and rain and a quantity of water
51 III,  1 |          and there results either rain, or, if the other exhalation
52 III,  1 |           be no snow or northerly rain, since these occur when
53 III,  3 |         in itself it is a sign of rain, but if it fades away, of
54 III,  3 |         it is naturally a sign of rain since it shows that a process
55 III,  3 |      carried to an end, result in rain. For the same reason these
56 III,  4 |    forming into raindrops but the rain is not yet actually there,
57 III,  4 |            it must either turn to rain or be dissolved, but opposite
58 III,  6 |       mock sun is a surer sign of rain than the rods; it indicates,
59 III,  6 |          south is a surer sign of rain than one to the north, for