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TROPICAL NATUREclimate of the equatorial zone are brought about, how it isthat so high a temperature is maintained during the absenceof the sun at night, and why so little effect is produced bythe sun's varying altitude during its passage from the northernto the southern tropic. In this favoured zone the heat isnever oppressive,as it so often becomes on the borders of thetropics; and the large absolute amount of moisture alwayspresent in the air is almost as congenial to the health of manas it is favourable to the growth and development of vegetation.1 Again, the lowering of the temperature at night is soregular and yet so strictly limited in amount, that, althoughnever cold enough to be unpleasant, the nights are never sooppressively hot as to prevent sleep. During the wettestmonths of the year, it is rare to have many days in successionwithout some hours of sunshine, while even in the driestmonths there are occasional showers to cool and refresh theoverheated earth. As' a result of this condition of the earthand atmosphere, there is no check to vegetation, and little ifany demarcation of the seasons. Plants are all evergreen;flowers and fruits, although more abundant at certain seasons,are never altogether absent; while many annual food-plantsas well as some fruit -trees produce two crops a year. Inother cases, more than one complete year is required tomature the large and massive fruits, so that it is not uncommonfor fruit to be ripe at the same time that the tree iscovered with flowers in preparation for the succeeding crop.This is the case with the Brazil nut tree in the forests of theAmazon, and with many other tropical as with a few temperatefruits.Uniformity of the Equatorial Climate in all Parts of the GlobeThe description of the climatal phenomena of the equatorialzone here given has been in great part drawn from longpersonal experience in South America and in the MalayArchipelago. Over a large portion of these countries thesame general features prevail, only modified by varying local1Where the inhabitants adapt their mode of life to the peculiarities ofthe climate, as is the case with the Dutch in the Malay Archipelago, theyenjoy as robust health as in Europe both in the case of persons born inEurope and of those who for generations have lived under a vertical sun.

I CLIMATE AND ASPECTS OF THE EQUATORIAL ZONE 231conditions. Whether we are at Singapore or Batavia, in theMoluccas or New Guinea, at Para, at the sources of theRio Negro, or on the Upper Amazon, the equatorial climateis essentially the same, and we have no reason to believe thatitmaterially differs in Guinea or the Congo. In certainlocalities, however, a more contrasted wet and dry seasonprevails, with a somewhat greater range of the thermometer.This is generally associated with a sandy soil, and a less denseforest, or with an open and more cultivated country. Theopen sandy country with scattered trees and shrubs or occasionalthickets, which is found at Santarem and Monte- Alegreon the lower Amazon, are examples, as well as the opencultivated plains of Southern Celebes ;but in both cases theforest country in adjacent districts has a moister and moreuniform climate, so that it seems probable that the nature ofthe soil or the artificial clearing away of the forests, areimportant agents in producing the departure from the typicalequatorial climate observed in such districts.Effects of Vegetation on ClimateThe almost rainless district of Ceara on the north-east coastof Brazil, and only a few degrees south of the equator, is a strikingexample of the need of vegetation to react on the rainfall.We have here no apparent cause but the sandy soil and barehills, which, when heated by the equatorial sun, produce ascendingcurrents of warm air and thus prevent the condensation ofthe atmospheric vapour, to account for such an anomaly ;andthere is probably no district where judicious planting wouldproduce such striking and beneficial effects. In Central Indiathe scanty and intermittent rainfall, with its fearful accompanimentof famine, is perhaps in great part due to theabsence of a sufficient proportion of forest -covering to theearth's surface ;and it isby a systematic planting of all thehill -tops, elevated ridges, and higher slopes that we shallprobably cure the evil. This would almost certainly inducean increased rainfall ;but even more important and morecertain is the action of forests in checking evaporation fromthe soil and causing perennial springs to flow, which may becollected in vast storage tanks and serve to fertilise a greatextent of country ;whereas tanks without regular rainfall or

TROPICAL NATUREclimate of the equatorial zone are brought about, how it isthat so high a temperature is maintained during the absenceof the sun at night, and why so little effect is produced bythe sun's varying altitude during its passage from the northernto the southern tropic. In this favoured zone the heat isnever oppressive,as it so often becomes on the borders of thetropics; and the large absolute amount of moisture alwayspresent in the air is almost as congenial to the health of manas it is favourable to the growth and development of vegetation.1 Again, the lowering of the temperature at night is soregular and yet so strictly limited in amount, that, althoughnever cold enough to be unpleasant, the nights are never sooppressively hot as to prevent sleep. During the wettestmonths of the year, it is rare to have many days in successionwithout some hours of sunshine, while even in the driestmonths there are occasional showers to cool and refresh theoverheated earth. As' a result of this condition of the earthand atmosphere, there is no check to vegetation, and little ifany demarcation of the seasons. Plants are all evergreen;flowers and fruits, although more abundant at certain seasons,are never altogether absent; while many annual food-plantsas well as some fruit -trees produce two crops a year. Inother cases, more than one complete year is required tomature the large and massive fruits, so that it is not uncommonfor fruit to be ripe at the same time that the tree iscovered with flowers in preparation for the succeeding crop.This is the case with the Brazil nut tree in the forests of theAmazon, and with many other tropical as with a few temperatefruits.Uniformity of the Equatorial Climate in all Parts of the GlobeThe description of the climatal phenomena of the equatorialzone here given has been in great part drawn from longpersonal experience in South America and in the MalayArchipelago. Over a large portion of these countries thesame general features prevail, only modified by varying local1Where the inhabitants adapt their mode of life to the peculiarities ofthe climate, as is the case with the Dutch in the Malay Archipelago, theyenjoy as robust health as in Europe both in the case of persons born inEurope and of those who for generations have lived under a vertical sun.

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