An Instrumented Golden Eagle's (Aquila chrysaetos) Long-Distance Flight Behavior.

One-second-processed three-dimensional position observations transmitted from an instrumented golden eagle were used to determine the detailed long-range flight behavior of the bird. Once elevated from the surface, the eagle systematically used atmospheric gravity waves, first to gain altitude, and then, in multiple sequential glides, to cover over 100 km with a minimum expenditure of its metabolic energy.

Understanding Animal Detection of Precursor Earthquake Sounds.

We use recent research to provide an explanation of how animals might detect earthquakes before they occur. While the intrinsic value of such warnings is immense, we show that the complexity of the process may result in inconsistent responses of animals to the possible precursor signal. Using the results of our research, we describe a logical but complex sequence of geophysical events triggered by precursor earthquake crustal movements that ultimately result in a sound signal detectable by animals. The sound heard by animals occurs only when metal or other surfaces (glass) respond to vibrations produced by electric currents induced by distortions of the earth's electric fields caused by the crustal movements. A combination of existing measurement systems combined with more careful monitoring of animal response could nevertheless be of value, particularly in remote locations.

Response of African elephants (Loxodonta africana) to seasonal changes in rainfall.

The factors that trigger sudden, seasonal movements of elephants are uncertain. We hypothesized that savannah elephant movements at the end of the dry season may be a response to their detection of distant thunderstorms. Nine elephants carrying Global Positioning System (GPS) receivers were tracked over seven years in the extremely dry and rugged region of northwestern Namibia. The transition date from dry to wet season conditions was determined annually from surface- and satellite-derived rainfall. The distance, location, and timing of rain events relative to the elephants were determined using the Tropical Rainfall Measurement Mission (TRMM) satellite precipitation observations. Behavioral Change Point Analysis (BCPA) was applied to four of these seven years demonstrating a response in movement of these elephants to intra- and inter-seasonal occurrences of rainfall. Statistically significant changes in movement were found prior to or near the time of onset of the wet season and before the occurrence of wet episodes within the dry season, although the characteristics of the movement changes are not consistent between elephants and years. Elephants in overlapping ranges, but following separate tracks, exhibited statistically valid non-random near-simultaneous changes in movements when rainfall was occurring more than 100 km from their location. While the environmental trigger that causes these excursions remains uncertain, rain-system generated infrasound, which can travel such distances and be detected by elephants, is a possible trigger for such changes in movement.

On the Possible Detection of Lightning Storms by Elephants.

Theoretical calculations suggest that sounds produced by thunderstorms and detected by a system similar to the International Monitoring System (IMS) for the detection of nuclear explosions at distances ≥100 km, are at sound pressure levels equal to or greater than 6 × 10(-3) Pa. Such sound pressure levels are well within the range of elephant hearing. Frequencies carrying these sounds might allow for interaural time delays such that adult elephants could not only hear but could also locate the source of these sounds. Determining whether it is possible for elephants to hear and locate thunderstorms contributes to the question of whether elephant movements are triggered or influenced by these abiotic sounds.

Long-distance, low-frequency elephant communication.

The production, transmission, and reception of and the behavioral response to long-distance, low-frequency sound by elephants is reviewed. The structure of low-frequency calls generated by elephants is separated into the "source" and the "filter" roles played by the lungs, larynx and vocal track, the composition of the expired air and the ambient air temperature. Implications regarding the size, age, sex, sexual and physical status follow from the call structure and detection. Reception of the signal is discussed in terms of the characteristics of the elephant's ear with particular attention to the determination of the threshold of hearing and the ability to locate the source of low-frequency sounds. Factors which influence the transmission of near infrasound are related to atmospheric structure. The critical role played by the thermal stratification and vertical gradient and magnitude of the wind in determining both the range and the detection of a signal are discussed for open and closed elephant habitats. Infrasound plays a pervasive role in reproduction, resource utilization, avoidance of predation and other social interactions. Current and future technology can be expected to contribute to the detection and interpretation of elephant communication. This will aid in the understanding of behavior and in efforts to sustain the species.

Ozone dynamics and deposition processes at a deforested site in the Amazon basin.

The goal of this study is to investigate the impact of deforestation on ozone dynamics and deposition in the Brazilian Amazon basin. This goal is accomplished through i) analyses of ozone levels and deposition rates at a deforested site during the rainy season; and ii) comparisons of these data with similar information derived at a forest. At the pasture site maximum ozone mixing ratios reach 20 parts per billion on a volume basis (ppbv) but about 6 ppbv prevail over the forest. Maximum ozone deposition velocities for pastures can reach 0.7 cm s-1, which is about threefold lower than values derived for forests. Combining ozone abundance and deposition velocities, pasture maximum ozone fluxes reach approximately 0.2 microgram (ozone) m-2 s-1. This flux represents approximately 70% of the deposition rates measured over the forest. Hence, this study suggests that conversion of rainforests to pastures could lead to a net reduction (30%) in the ozone sink in the Amazon.

The role of the atmosphere in fire occurrence and the dispersion of fire products

It provides background and predictive information on the occurrence of large fires and the transport of their products. Document in pdf format; Acrobat Reader required.

Análise da variabilidade diária da precipitação em área de pastagem para a época chuvosa de 1999 - projeto TRMM/LBA

As part of the investigations of the experiment TRMM/LBA in Amazônia, measurements of the rain were obtained in a pasture site. In this work precipitation distribution were analyzed during the period from January 10 to February 28, 1999 (wet season). The monthly totals of precipitation for the period were 322.3 and 468.6 mm for January and February, respectively. The analyses of the frequency distribution for the events lower than 1 mm.h-1 and higher than 1, 3, 5, 10, 15 and 20 mm.h-1 showed different time distribution. The events lower than 1 mm.h-1 presented a more regular temporary distribution, even representing only 3% of the total volume of precipitation (27 mm). The events with precipitation above 1, 3, 5 mm.h-1 presented a similar pattern among them, and the most frequent cases ocurred during late afternoon. Those events represented about 97, 91 and 86% of the total of the precipitation, respectively. Finally, the events above 10, 15 and 20 mm.h-1 represented 73, 68 and 62% of the total of the precipitation respectively, and the largest relative frequencies concentrated among 2 up to 4 HL and 15 up to 17 HL. The rainfall observed can be classified in 2 distint system: local convection and mesoscale convective system, which provoke peaks at 16 LT and 4 LT, respectively.

Como parte das investigações do experimento TRMM/LBA na Amazônia, medidas de chuva foram obtidas continuamente sobre uma área de pastagem. Neste trabalho foram analisados dados de precipitação durante o período compreendido entre 10 de janeiro a 28 de fevereiro de 1999 (período chuvoso). Os totais mensais de precipitação para o período estudado foram de 322,3 e 468,6 mm para janeiro e fevereiro, respectivamente. As análises da distribuição de frequência para os eventos inferiores a 1 mm/h e superiores a 1, 3 , 5, 10, 15 e 20 mm.h-1, mostraram diferentes distribuição temporal. Os eventos inferiores a 1 mm.h-1 apresentaram uma distribuição temporal mais regular, porém representando apenas cerca de 3% do volume total de precipitação (27 mm). Os eventos com precipitação superiores a 1, 3, 5 mm.h-1 apresentaram um padrão similar entre si, sendo que os casos mais frequentes ocorreram durante a madrugada e final da tarde. Esses eventos representaram cerca de 97, 91 e 86% do total da precipitação, respectivamente. Finalmente, os eventos acima de 10, 15 e 20 mm.h-1 totalizaram, respectivamente, 73, 68 e 62% do total da precipitação, e as maiores frequências relativas concentraram-se entre 2 às 4 HL e 15 às 17 HL. A precipitação observada pode ser classificada em 2 sistemas distintos de produção de chuva: convecção isolada local e sistemas convectivos de mesoescala, os quais provocaram máximos de precipitação às 16 e 4 HL, respectivamente.