CHAP. XV.

CLIMATE OF CHINA.—SUMMER AND WINTER.—TEMPERATURE OF HONG-KONG—OF SHANGHAE.—MONSOONS.—TYPHOONS.—SIGNS OF THEIR APPROACH.—DESCRIPTION OF A TYPHOON WITNESSED BY THE AUTHOR.—EFFECT PRODUCED UPON VEGETATION.—RAINS.—WET AND DRY SEASONS.—METEOROLOGICAL TABLE.

In order to understand Chinese agriculture, a knowledge of the climate of the country is of course necessary. The dominions of the Emperor of China stretch over twenty-three degrees of latitude—from 18° to 41° north, and from the 98° to the 123° of east longitude; thus including both tropical and temperate regions in its vast extent. Being placed on the east side and forming part of the large continent of Asia, it is liable to extremes of temperature—to excessive heat in summer, and extreme cold in winter—which are unknown in many other parts of the world within the same parallels of latitude. One of our best writers upon China[1] makes the following very sensible remarks on this subject:—"Although Peking is nearly a degree to the south of Naples—the latitude of the former place being 30° 54', of the latter 40° 50'—the mean temperature of Peking is only 54° of Fahrenheit, while that of Naples is 63°. But the thermometer at the Chinese capital sinks much lower during the winter than at Naples, so in summer does it rise somewhat higher; the rivers are said to be frozen for three or four months together, from December to March; while during the last embassy in September, 1816, we experienced a heat of between 90° and 100° in the shade. Now it is well known that Naples, and other countries in the extreme south of Europe, are strangers to such a degree of long-continued cold, and not often visited by such heats. "Europe," observes Humboldt, "may be considered altogether as the western part of a great continent, and therefore subject to all the influence which causes the western sides of continents to be warmer than the eastern; and at the same time more temperate, or less subject to excesses of both heat and cold, but principally the latter."

From my own tables, kept by Newman's best registering thermometers, I find that at Hong-kong, in the months of July and August—the two hottest months in the year—the mercury frequently stood as high as 90°, and one day at 94° Fahr. in the shade. The minimum was generally about ten degrees lower than the maximum. In the winter, from December to March, the thermometer frequently sinks nearly down to the freezing point, and sometimes, although rarely, snow has fallen at Canton and on the adjacent hills. The influence of the sea, however, in this part of the empire, has a tendency to check the extremes of both heat and cold; but these are much greater in the northern interior. The northerly winds in the winter and spring months are severely cold in the south of China; indeed, I have suffered more from cold at Hong-kong and Macao in the month of February, than I have ever done in England.

At Shanghae, in the province of Keangsoo, in latitude 31° 20' north, the extremes of heat and cold are much greater than what we experienced in the southern provinces. Through the kindness of Dr. Lockhart, who kept up my meteorological tables during my absence in different parts of the country, I have obtained a very complete set of observations for nearly two years. From these it appears that in July and August the heat is the greatest; the thermometer in the shade sometimes standing for several days at 100° of Fahrenheit. The heat during these days was almost insupportable to Europeans, who, when I was in Shanghae, were obliged to live in Chinese houses, which, from their construction, were ill calculated to exclude the heat. In the end of October the thermometer sometimes sinks as low as the freezing point. In the evening of the 28th of that month, in 1844, the remains of the cotton and other tropical plants which are cultivated in the fields during the summer, were destroyed by frost. December, January, and February are the coldest months in the year, the cold then being quite as severe as it is with us in the south of England. In the winter of 1844–45 the thermometer sunk as low as 26° Fahrenheit. On the night of the 18th of December, and again on January, the 4th, the index was left at 24°. But that winter, according to Chinese accounts, was peculiarly mild, so much so, that the usual supply of ice could not be procured. In ordinary years the ponds and canals are frequently frozen several inches in thickness, and afford a plentiful supply of ice. I have, therefore, little doubt that in most years the thermometer may be found at least twenty degrees below the freezing point, or at 12° of Fahrenheit, and perhaps even lower. Snow frequently falls, but the sun is too powerful to allow it to lie long on the ground.

If we except the extremes of heat and cold just noticed, the climate of Shanghae may be pronounced as fine as any in the world. Even the cold in winter is highly advantageous to the natives, and still more so to Europeans and Americans, as it strengthens their constitutions, and enables them to withstand the effects of the excessive heat. The months of April, May, and June are delightful, and although the sun is hot in the middle of the day, in the afternoon the air is soft and agreeable, and the evenings cool and pleasant. The autumnal months are generally of the same description; the wind then is cool and bracing, and the sky is much clearer than in England. The sun, for days, and sometimes for weeks together, rises in the morning, runs his course, and sets again in a clear and cloudless sky.

The prevailing winds blow from the south-west from the end of April to the middle of September; during the remaining portion of the year they are northerly and easterly: thus forming what are called the south-west and north-east monsoons. These monsoons blow with great regularity in the south of China, but are more variable towards the north. In the latitude of Chusan or Shanghae, although the monsoons prevail, the wind, not unfrequently, blows from other quarters. In the end of the summer season, that is, from July to October, the country is frequently visited by those dreadful gales called by foreigners typhoons. The name is a corruption of the Chinese word Ta-fung or "great wind." These storms commit the most fearful ravages both by land and sea. The barometer gives warning some hours before the gale commences, and, therefore, foreign ships can always send down their masts and yards, and, if possible, remove to a safe anchorage. Where that is not to be had, they have the dreadful alternative of standing out to sea. The Chinese, without the aid of the barometer, can always tell when the Ta-fung is coming on by the following signs. The wind, which blows from the south-west in the typhoon season, changes and blows from the north or north-cast, becoming gusty and gradually increasing in strength, the sky lowers and looks wild, the sea rolls in upon the bench with a dead heavy swell, and every thing portends a coming storm. When these signs appear, the fleets of fishing-boats on the coast take their nets in, crowd all sail, and make for the shore as fast as they can, where the boats are hauled up on dry land, or into some creek which is sheltered from the force of the winds and waves. The coasting junks, which are ill fitted for bad weather, lose no time in getting into some sheltered port where they can ride out the storm in safety. And, luckily, as a safeguard from the fury of these winds, nature has provided a great number of excellent well-sheltered harbours on the coast of China, all of which are well known to the pilots who are employed on board the junks.

During my residence in China, I witnessed two of these terrific gales—once at sea, and once on shore. Luckily, in the first instance, we were able to run into a deep bay, and with three anchors down rode out the gale in perfect safety. The other occurred on the 21st and 22d of August, 1844, when I was at Ningpo. I observed the Chinese running about in great consternation, and calling to each other that the "great wind" was coming, and to make preparations for it. Mats and rattan work, which had been placed over the doors and windows to afford shade from the sun, were hastily removed, and many of the houses, which were known to be in a weak state, were, in a rapid way, propped up and strengthened. Nor were the husbandmen less busy in the fields. The heads of the tall millet, being nearly ripe, were quicky cut, and the long stalks left to be reaped at another time. Millet is so heavy when nearly ripe, that had it been left exposed to the wind it must have been dashed to pieces, and the crop entirely lost. Crops on the sides of the rivers and canals were removed where it was possible to do so; otherwise, they would have been blown into the water, and carried away far beyond the reach of their owners. All the fruit which was nearly ripe was hastily gathered from the trees, unnecessary branches were cut away, and others tied up and supported.

The gale gradually increased in force until daylight on the morning of the 22d, when it seemed to be at its height. In Mr. Mackenzie's house, where I was staying at the time, we passed a fearful night. The wind howled and whistled round the roof, every blast seemingly more fierce than that which preceded it, until I really thought we should have the building down upon us and be buried in the ruins. At daylight the rooms presented a dismal appearance; all the floors, chairs, and tables were covered with dust and pieces of broken tiles and mortar which had been shaken out of the roof. As the storm still raged with unabated fury, Mr. Mackenzie and myself, glad to escape from the wreck by which we were surrounded, went out to see what effect the gale was producing on the other places in the vicinity. The wind was so powerful, that it was next to impossible to keep our feet; in fact, we were frequently blown off the path, and were obliged to scramble back to it again on our bands and knees. The river, which is generally beautiful and smooth, had now risen and completely overflowed its banks, having been forced back by the strength of the wind, and was as rough as the sea itself. The whole country was one vast sheet of troubled water, for the branches of the river, and the numerous canals by which it is intersected, had all overflowed their banks, and had spread in the low paddy fields. Most of the small boats were safe, as they were either in sheltered creeks, or drawn up beyond the reach of the water, but many of the large wood-junks which frequent this port were not so fortunate. These had been moored off the city, having, as usual, a large portion of their cargo lashed to their sides. In many instances, the combined force of the winds and waves snapped the lashings, strong as they were, and the spars of wood floated from their sides, and were either carried away by the force of the stream, or thrown on shore. Hundreds of the Chinese were now ready to seize the wood as it floated to land, and with a total disregard to the "rights of property" conveyed it at once to their own houses. No Mandarin or other government officer interfered to prevent this, and the Chinese servants of the English Consul and other foreign residents actually brought a considerable quantity to the houses of their masters, and seemed surprised when reproved for their dishonesty. The English of course honourably returned the spoil to its owners, much to the surprise of the Chinese. On the opposite side of the river, we observed great numbers engaged in the same lawless occupation. The city walls, here, run parallel with the river, and these rascals were coolly hoisting the wood over the wails and ramparts, assisted by their friends inside the city; nor was this attempted to be checked.

At about nine o'clock in the morning, the wind, which commenced from the north, had veered round to the east and south, but still raged with fearful power. On retracing our steps, which we had some difficulty in doing, owing to the flooded state of the country, and the force of the wind, we encountered a family group in the fields surrounding a coffin, which the wind seemed inclined to carry off in spite of all their efforts to fasten it to the ground. It is customary in this part of the country to place the remains of the dead upon the surface of the ground, sometimes supporting the coffins on short stakes, to raise them a few feet from the earth. In this instance the poor people were actually fighting with the winds, but were at last able to secure the remains of their relative, and allow him to sleep the long sleep of death in peace. At this time the barometer stood at 28° 30', but the wind was still blowing a perfect gale until about mid-day, when it gradually became less violent. In the evening, although the sky still looked wild, it was evident the gale had passed away, and the wind was then blowing from the south-west. The river soon returned to its former limits, boats began to sail up and down, and business, which had been entirely suspended, went on again as usual. Altogether, the typhoon lasted nearly twenty-four hours.

The following morning was calm and beautiful, but the scene was one of ruin and devastation. The streets were strewed with broken tiles and mortar; many of the houses were completely unroofed, walls were blown down, and every thing evinced the violence of the storm. In the fields the change was still more striking; but two days before the trees and hedges were green, the gardens were gay with flowers, and every thing bore the happy smiling aspect of summer; now vegetation had changed from green to withered sickly brown, flowers had faded, trees were torn lip by the roots and broken and shattered, and many of the crops were completely ruined.

The accounts which reached us from sea after this typhoon proved that the loss of life had been very great. For many days after the gale had ceased, our vessels on the coast frequently met with large portions of wreck floating about, the remains of Chinese junks, which told a fearful tale. An English vessel on her way to Chusan was obliged to cut away her masts, and was towed into the harbour a day or two afterwards by one of the government steamers. Mr. Shaw, one of her passengers, informed me that during the typhoon they had a perfect calm for some time, and that then the wind veered round to a different quarter, and blew with increased violence. This is not unfrequently the case, and during these short lulls the vessels roll and labour in a dreadful manner, owing to the heavy swell of the sea, as they are then entirely at its mercy, and have nothing to steady them.

In the preceding year, this part of the country was twice visited by typhoons, viz., on the 1st of September and 1st of October. In the island of Chusan, where they were particularly violent, the most disastrous effects were produced upon the crops. The little streams in the island were swollen into large rivers, and carried away every thing before them. The crops of entire fields, chiefly paddy, were in some instances swept away, and in others sanded completely up, and rendered useless. The patched-up houses of our officers who held the island at the time suffered severely. During the typhoon of 1844, a house built on the beach by one of the officers was actually lifting up, and would doubtless have been carried away by the force of the wind, but fortunately Brigadier Campbell, who was passing at the time, gave the alarm, and ordered out a number of men from the barracks, who held it down until it was rendered more secure.

The wet and dry seasons in the southern and tropical parts of China are more decided in their character than they are in the northern portions of the Empire. At Hong-kong and in the provinces of the south, the winter season, that is, from October to March, is generally dry, more particularly in November, December, and January. The most wet months in the year are those near the change of the monsoons, in May and June, and again in September, when the rains fall in torrents, probably owing to the stagnation produced in the atmosphere by the change in the direction of the winds.

The author before quoted explains this on the following principles. He says:—"The north-east monsoon, which commences about September, blows strongest during the above period, and begins to yield to the opposite monsoon in March. About that time the southerly winds come charged with the moisture which they have acquired in their passage over the sea through warm latitudes; and this moisture is suddenly condensed into thick fogs as it comes in contact with the land of China, which has been cooled down to a low temperature by the long-continued northerly winds. The latent heat given out, by the rapid distillation of this steam into fluid, produces the sudden advance of temperature which takes place about March; and its effect is immediately perceptible in the stimulus given to vegetation of all kinds, by this union of warmth with moisture. With the progressive increase of heat and evaporation those rains commence, which tend so greatly to mitigate the effects of the sun's rays in tropical climates. In the month of May the fall of rain has been known to exceed twenty inches, being more than a fourth of all the year, and this keeps down the temperature to the moderate average marked for that month."

The following table made from observations kept by the late Mr. Beale at Macao for a number of years, shows the amount of the average monthly fall of rain in inches:—

Thermometer.Mean
Height of
Barometer.
Average Fall
of Rain
in Inches.
Mean
Max.
Mean
Min.
Mean
Temp.
Range.
FromTo
January
February
March
April
May
June
July
August
September
October
November
December
57
58
71
76
78
84
88
86
84
76
68
63
45
45
60
69
73
79
84
83
79
70
61
52
51
51.5
65.5
72.5
75.5
81.5
86
84.5
81.5
73
64.5
57.5
65
68
79
84
86
89
94
90
88
85
79
69
29
33
45
59
69
74
81
79
75
60
48
40
30.23
30.12
30.17
30.04
29.89
29.87
29.84
29.86
29.90
30.04
30.14
30.25
0.675
1.700
2.150
5.675
11.850
11.100
7.750
9.900
10.925
5.500
2.425
0.975
Annual Means74.166.770.481.357.630.03

Total rain, 70.625

In the north the rains also fall copiously at the change of the monsoons, more particularly in spring, at which time they are of the greatest utility to the crops, which are sown or planted about that time. Those parts of China, however, which are included in the temperate zone, cannot properly be said to have a wet and dry season in the same sense as these terms are generally understood in the tropics. The winter months which are dry at Hong-kong are far from having the same character, at Shanghae, for example, where heavy and continued falls of rain and snow are of frequent occurrence. In fact, the climate of Northern China has a greater resemblance to that of the south of England or France, than it has to that of the southern parts of the Chinese empire; and although hotter, used always to remind me of the beautiful summers we have in England once in every ten and twelve years. The sky is for days and weeks together without a cloud, and in the evening a heavy dew falls and refreshes vegetation.

These remarks will assist the reader to understand more fully the theory and practice of Chinese agriculture, which form the subject of the following chapter.

[1] Davis's "Chinese."