Civic Discipline: Geography in America, 1860-1890

Civic Discipline argues that the story of the origins of American geography is a distinctly "New York story." Wealthy businessmen began America's first geographical society - the American Geographical Society - in 1851, inspired by what geographical knowledge of the globe could offer an expanding American commercial Empire at home and abroad. AGS meetings were spectacularly popular among the public and press. At them, geography was cast as a science in the service of the public and civic good. Meanwhile though, AGS men's spatial and financial "missions" became closely linked. They helped improve derelict spaces in New York City and weighed in on controversial scientific questions of the day in the Arctic, yet the geographical knowledge they advanced - such as in the American West and in Central Africa - also created enormous personal wealth. Civic Discipline shows that it was not just that historical events shaped geography, but rather, that geography shaped historical events.

Recent increase in black carbon concentrations from a Mt. Everest ice core spanning 1860-2000 AD

A Mt. Everest ice core spanning 1860–2000 AD and analyzed at high resolution for black carbon (BC) using a Single Particle Soot Photometer (SP2) demonstrates strong seasonality, with peak concentrations during the winter-spring, and low concentrations during the summer monsoon season. BC concentrations from 1975–2000 relative to 1860–1975 have increased approximately threefold, indicating that BC from anthropogenic sources is being transported to high elevation regions of the Himalaya. The timing of the increase in BC is consistent with BC emission inventory data from South Asia and the Middle East, however since 1990 the ice core BC record does not indicate continually increasing BC concentrations. The Everest BC and dust records provide information about absorbing impurities that can contribute to glacier melt by reducing the albedo of snow and ice. There is no increasing trend in dust concentrations since 1860, and estimated surface radiative forcing due to BC in snow exceeds that of dust in snow. This suggests that a reduction in BC emissions may be an effective means to reduce the effect of absorbing impurities on snow albedo and melt, which affects Himalayan glaciers and the availability of water resources in major Asian rivers.

Jane Addams (1860-1935): Social worker and Peace Builder

The name Jane Addams is typically associated with the Settlement House Movement. As a founder of Hull House, the first settlement house in the United States, Addams worked tirelessly on behalf of the poor and oppressed. Less widely known is the depth of her concern about peace and her efforts as a peace builder. A more careful review, however, of Addams’ words and works reveals her passionate commitment to the abolition of war and the restoration of peace. This biographical sketch highlights the breadth and depth of Addams’ work both as an advocate for the poor and as an advocate for peace.

Edna Chamberlain (1921 -2005): A Leader through Times of Transition and Change

Professor Edna Chamberlain was an outstanding leader in Australian social work. She contributed extensively to social work education at the University of Queensland, the social work profession through her leadership of the Australian Association of Social Workers and to the community through advocacy for progressive social policies. Her life experiences were influential is shaping her career and her particular teaching and research interests. Early in her life, Chamberlain was exposed to individual deprivation as a result of the Great Depression. This provided the incentive for a career in social work. She worked as a social work practitioner for some years and entered the academic world until after the death of her husband. In the university and profession, she was confronted by conflict between traditionalists and those wanting immediate reform. In managing these tensions, she tried to find the common ground but these tensions also moderated and changed her views about the purpose and practice of social work. Her rich practice and later research and teaching background provided a strong basis for her professional leadership, research activities and curriculum initiatives. Whilst social casework methods were influential early in her career she sought in later years to integrate the private pain of individuals with social policy and community planning by focusing on the purpose of social work – demonstrating her commitment to the disadvantaged in the context of social justice.

Recent Increase in Black Carbon Concentrations from a Mt. Everest Ice Core Spanning 1860-2000 AD

A Mt. Everest ice core spanning 1860-2000 AD and analyzed at high resolution for black carbon (BC) using a Single Particle Soot Photometer (SP2) demonstrates strong seasonality, with peak concentrations during the winter-spring, and low concentrations during the summer monsoon season. BC concentrations from 1975-2000 relative to 1860-1975 have increased approximately threefold, indicating that BC from anthropogenic sources is being transported to high elevation regions of the Himalaya. The timing of the increase in BC is consistent with BC emission inventory data from South Asia and the Middle East, however since 1990 the ice core BC record does not indicate continually increasing BC concentrations. The Everest BC and dust records provide information about absorbing impurities that can contribute to glacier melt by reducing the albedo of snow and ice. There is no increasing trend in dust concentrations since 1860, and estimated surface radiative forcing due to BC in snow exceeds that of dust in snow. This suggests that a reduction in BC emissions may be an effective means to reduce the effect of absorbing impurities on snow albedo and melt, which affects Himalayan glaciers and the availability of water resources in major Asian rivers. Citation: Kaspari, S. D., M. Schwikowski, M. Gysel, M. G. Flanner, S. Kang, S. Hou, and P. A. Mayewski (2011), Recent increase in black carbon concentrations from a Mt. Everest ice core spanning 1860-2000 AD, Geophys. Res. Lett., 38, L04703, doi: 10.1029/2010GL046096.