Conservation is a long-term process that unfolds over time and seeks to develop harmony between human activity and ecosystems of all types. The unfolding of conservation in the Luquillo Mountains of Puerto Rico took place over a period of over 140 years, beginning in 1876. The conservation process in Puerto Rico involved the description of the biodiversity, the understanding of forest dynamics in relation to the conditions prevailing in the Luquillo Mountains, extensive research on the life history of critical species, understanding the basis of forest resilience, recognizing the social-ecological-technological context of conservation, applying advanced technological tools, and resolving the inevitable conflict that develops among the different actors involved in the conservation effort. Unfolding conservation within a country requires continuous and effective support from governmental, non-governmental, business, and scientific sectors of the social-ecological-technological systems of the country. These sectors come together at different moments in time, and the path followed is different in different countries. In Puerto Rico, the unfolding of conservation was triggered by the government in close collaboration with academic and governmental scientific sectors. Within the Luquillo Mountains, the business sector did not oppose conservation activities, and the unfolding process reached high levels of effectiveness. The rest of Puerto Rico benefited from the conservation process unfolding on the Luquillo Mountains. In contrast, conservation in the Amazon has been characterized by conflict among different actors competing for a common resource. In general, commercial activities that are based on resource exploitation lead to conflict and a slower development of conservation activities. When the business community used science to improve land productivity, as it did in Central America, conservation benefited because the science that was used stimulated conservation values. The establishment of government institutions with a focus on conservation through research and education appeared late in the mainland tropics compared to Puerto Rico, but when it happened, it accelerated the unfolding of conservation. All the countries examined here were most effective in conservation when the collaboration among the different sectors of society was high and based on objective and anticipatory scientific activity.
Article
Conservation in the Luquillo Mountains of Puerto Rico
Ariel E. Lugo
Article
The History and Science of Hurricanes in the Greater Caribbean
Sherry Johnson
The Caribbean’s most emblematic weather symbol is the hurricane, a large rotating storm that can bring destructive winds, coastal and inland flooding, and torrential rain. A hurricane begins as a tropical depression, an area of low atmospheric pressure that produces clouds and thunderstorms. Hurricane season in the Caribbean runs from June 1 through November 30, although there have been infrequent storms that formed outside these dates. Hurricanes are classified according to their maximum wind speed, and when a tropical system reaches the wind speed of a tropical storm (35 mph), it is given a name. Lists of names, which are rotated periodically, are specific to certain regions. If a named storm is responsible for causing a significant number of deaths or property damage, the name is retired and replaced with another.
Most deaths in a storm came from drowning, from storm surge along the coast or from flooding or mudslides in the interior. Storm-related deaths also occur when structures collapse or when victims are struck by flying debris. One important and underestimated cause of death after the passage of a storm is disease. Even if the destruction is not immediate, the passage of a hurricane can leave significant ecological damage along the coast and in the interior.
Hurricanes can have a devastating effect on a community that takes a direct hit. Repeated hurricane strikes can leave a sense of helplessness and hopelessness, “hurricane fatigue.” Conversely, survivors of a disaster are often left with a feeling of confidence that, since they have endured the effects of at least one deadly hurricane, they can do so again.
Until the last half of the 18th century, meteorology remained primitive, but the Age of Enlightenment brought scientific and ideological advances. Major beneficiaries were royal navies whose navigation manuals and nautical charts became increasingly more accurate. In 1821, William C. Redfield established the circular nature of storms and their counterclockwise rotation, while other scientists showed how wind currents within the storms moved upward. Once the coiled structure of hurricanes were established by mid-century, the term “cyclone” was applied, based upon the Greek word for the coils of a snake.
After the mid-19th century, scientists moved from information gathering to attempts to predict hurricane strikes. Technology, in the form of the telegraph, was a key component in creating a forecasting system aided by organizations such as the Colegio de Belén, in Havana, Cuba. Later in the century, governments worldwide created official observation networks in which weather reports were radiotelegraphed from ships at sea to stations on land. The 20th century experienced advances, such as the use of kites and balloons, and the introduction of weather reconnaissance aircraft during World War II. In April 1960, the first satellite was launched to observe weather patterns, and by the early 1980s, ocean buoys and sophisticated radar systems made forecasts increasingly more accurate.
