The late author Sheldon H. Harris in his book " Factories of Death: Japanese Biological Warfare, 1932-1945, and the American cover up " wrote that, The test program, could be part of Project AGILE or Project OCONUS which began in fall 1962 and which was funded at least through fiscal year 1963, was considered by the Chemical Corps to be “ an ambitious one .” The tests were designed to cover “ not only trials at sea, but Arctic and tropical environmental tests as well .” The tests, presumably, were conducted at what research officers designated, but did not name, “ satellite sites .” These sites were located both in the continental United States and in foreign countries.

These species are found throughout tropical and subtropical South and Central America.

These tropical jungles are similar to coral reefs in that they are highly efficient at conserving and circulating necessary nutrients, which explains their lushness in a nutrient desert.

The most commonly used form of the Köppen classification has five primary types labeled A through E. These primary types are A, tropical ; B, dry ; C, mild mid-latitude ; D, cold mid-latitude ; and E, polar.

These 26 major types can be reclassified into 6 broader categories: temperate needleleaf ; temperate broadleaf and mixed ; tropical moist ; tropical dry ; sparse trees and parkland ; and forest plantations.

These mountains are recognised by biogeographers as the boundary between two of the Earth's great ecozones: the temperate Palearctic that covers most of Eurasia and the tropical and subtropical Indomalaya ecozone which includes the Indian subcontinent, Southeast Asia and Indonesia.

These fact determine that the southern coast have a semi Mediterranean desert like climate yet there is small variations between temperatures during night time or day time, as regions in tropical latitudes.

These forests have the particularity of connecting to the Amazon basin through the Marañon passage ( an area where there are also tropical dry forests ).

These species are found in disjunct tropical regions of South America ( one species ), Central Africa ( three species ) and Southeast Asia ( 25 species ).

These depths and times are typical of experienced sport divers leisurely exploring a coral reef using 200 bar aluminum cylinders rented from a commercial sport diving operation in most tropical island or coastal resorts.

These dates coincide with the hypothesis derived from fossils that the walrus evolved from a tropical or subtropical ancestor that became isolated in the Atlantic Ocean and gradually adapted to colder conditions in the Arctic.

These spiraling columns of air frequently develop in tropical areas close to the equator, and are less common at high latitudes.

These tropical perennials are grown for their ornamental foliage. They are mostly natives of tropical America.

These fertile plains consist of tropical seasonal moist deciduous, dry deciduous forests, and both dry and wet savannas that are home to chital, hog deer, barasingha, Indian sambar, and Indian muntjac.

These measurements can be used to locate weather fronts, monitor the El Niño-Southern Oscillation, determine the strength of tropical cyclones, study urban heat islands and monitor the global climate.

These extratropical convergence zones are occupied by the polar fronts where air masses of polar origin meet and clash with those of tropical or subtropical origin.

These forests also act as barriers against cyclones, tropical storms and tidal waves thus protecting the nearby villages.

These varieties form important components of pastures in many tropical regions.

These are typical lowland plants, growing in the tropical and subtropical zones of the paleotropics, from West Africa to the Pacific Islands.

These trees are characteristic features of many American tropical rainforest ecosystems and may be among the dominant tree species in some places.

These writings, known under the name of " pukapuka whakapapa " ( genealogy books, Māori ) or in tropical Polynesia as " puta tumu " ( origin stories ) or " puta tūpuna ” ( ancestral stories ) were jealously guarded by the heads of households.

These storms can have maximum winds extending farther from the center than in a purely tropical cyclone and have no weather fronts linking directly to the center of circulation.

These systems may also be described as " mid-latitude cyclones " due to their area of formation, or " post-tropical cyclones " where extratropical transition has occurred, and are often described as " depressions " or " lows " by weather forecasters and the general public.

These tropical cyclones would be given identifiers starting with SL in the future.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These prevailing winds blow from the west to the east, and steer extratropical cyclones in this general manner.

These prevailing winds blow from the west to the east, and steer extratropical cyclones in this general manner.

These systems may also be described as " mid-latitude cyclones " due to their area of formation, or " post-tropical cyclones " where extratropical transition has occurred, and are often described as " depressions " or " lows " by weather forecasters and the general public.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These tropical cyclones were only tropical storms on the Saffir-Simpson Hurricane Scale at their peak.

These dates conventionally delimit the period of each year when most tropical cyclones form in the northeastern Pacific Ocean.

These warm core cyclones tend to form over the oceans between 10 and 30 degrees of the equator.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.

These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin.