Social ecology of bottlenose dophins in Monterey Bay, California

Between 1990 and 1995, Pacific coastal bottlenose dolphins (Tursiops truncatus gillii) were studied using photo-identification during 228 boat-based surveys of the coastal strip (<1 km offshore) between Marina and New Brighton Beach in Monterey Bay (18 km of coastline). The study period encompassed 3 regular (1990, 1991 and 1995) and 3 El Niño years (1992, 1993, 1994). Based on dorsal fin markings, 97 unique individuals were identified. Eighteen animals (19%) showed a high level of site fidelity (defined as presence in at least 5 of the 6 years), although their overall range was larger than the study area. Thirty-eight animals (39%) were transient, leaving for periods of time, and 41 (42%) were occasional encounters. The rate of discovery indicated a pulsed recruitment of new individuals into the study area, with periods of stable school composition, especially during non-El Nino years, and periods of high school fluidity. Encounter rate was significantly higher in El Niño (81%) than non-El Niño years (61%). School size averaged 16 individuals (C.I.3, =0.05) and was significantly larger in El Niño years. Schools where calves were present were twice as large (mean=15; S.D.=8) than schools without calves (mean=8; S.D.=6). Newborns represented 12% of the sightings and were seen year round with a peak in summer and fall. Crude birth rate ranged between 0.09 and 0.17 (mean=0.13; S.D.=0.03). Five females calved in consecutive years and a resident female calved once a year for the duration of the study, possibly indicating a high rate of mortality for calves in this area. Individuals often traveled as subgroups of more consistent composition than the school itself, possibly indicating that a stronger social bond exists within these units which may function as “bands” (sensu Wells 1991) of same sex individuals traveling within a larger school of mixed composition. (ppt file of poster)

Numerical modeling of the propagation environment in the atmospheric boundary layer over the Persian Gulf

Strong vertical gradients at the top of the atmospheric boundary layer affect the propagation of electromagnetic waves and can produce radar ducts. A three-dimensional, time-dependent, nonhydrostatic numerical model was used to simulate the propagation environment in the atmosphere over the Persian Gulf when aircraft observations of ducting had been made. A division of the observations into high- and low-wind cases was used as a framework for the simulations. Three sets of simulations were conducted with initial conditions of varying degrees of idealization and were compared with the observations taken in the Ship Antisubmarine Warfare Readiness/Effectiveness Measuring (SHAREM-115) program. The best results occurred with the initialization based on a sounding taken over the coast modified by the inclusion of data on low-level atmospheric conditions over the Gulf waters. The development of moist, cool, stable marine internal boundary layers (MIBL) in air flowing from land over the waters of the Gulf was simulated. The MIBLs were capped by temperature inversions and associated lapses of humidity and refractivity. The low-wind MIBL was shallower and the gradients at its top were sharper than in the high-wind case, in agreement with the observations. Because it is also forced by land–sea contrasts, a sea-breeze circulation frequently occurs in association with the MIBL. The size, location, and internal structure of the sea-breeze circulation were realistically simulated. The gradients of temperature and humidity that bound the MIBL cause perturbations in the refractivity distribution that, in turn, lead to trapping layers and ducts. The existence, location, and surface character of the ducts were well captured. Horizontal variations in duct characteristics due to the sea-breeze circulation were also evident. The simulations successfully distinguished between high- and low-wind occasions, a notable feature of the SHAREM-115 observations. The modeled magnitudes of duct depth and strength, although leaving scope for improvement, were most encouraging.

Der Glaube versetzt Berge! Sozialpsychologische Effekter der Suche nach der Gerechtigkeit Gottes

Mit Kuno verbindet mich nicht allein das lnteresse an einer Theorie der Religion (Füssel, Huber, & Walpen, 1990). Mit dieser allerdings habe ich mich in den letztenJahren am intensivsten auseinandergesetzt. Daher erscheint es mir sinnvoll, zu dieser Thematik meinen Beitrag zu seiner Festschrift zu leisten. Kurzgefasst geht es darin um prosoziale Effekte religiôser Konstruktsysteme. Es lasst sich namlich zeigen, dass sie einen ideologischen Mechanismus zu neutralisieren vermôgen, wenn sie einen determinierenden Einfluss auf das Verhalten ausüben. Dabei spielt der Glaube, der nach einem allseits bekannten Diktum sogar Berge versetzen kann, eine entscheidende Rolle. Daher lese ich in dem Oberthema der Festschrift einen «Genitivus subjectivus». Es lautet dann: Suchet zuerst die Gerechtigkeit, die Gott realisiert bzw. realisieren wird. lch beginne mit der Darstellung einer sozialpsychologischen Theorie, die zu erklaren versucht, warum Menschen, die von einem ungerechten Ereignis getroffen werden, zu allem Überfluss auch noch die Schuld daran in die Schuhe geschoben bekommen. ln einem zweiten Schritt definiere ich, was ich unter religiôsen Konstruktsystemen verstehe und wie sie in sozialwissenschaftlichen Studien gemessen werden kônnen. Darauf aufbauend versuche ich zu prazisieren, wie religiôse Konstruktsysteme den Mechanismus der Schuldzuschreibung beeinflussen. Dazu greife ich aufDaten zurück, die ich 1999 in einer eigenen Untersuchung mit einer reprasentativen Stichprobe von Studierenden der Universitat Freiburg im Uechtland erhoben habe.