The research presented here documents institutional and organizational factors affecting fire management on tribal lands. Two case studies of fires occurring on tribal lands in Arizona provide insights into how these factors converged to influence the course of events. This study considers historic as well as current conditions and events because these affect whether or not people are receptive to information, to planning, and to working together. Though it focuses on decision making within tribes and agencies responsible for tribal lands, its findings are relevant for other locations as well.

As a major component of the Climate Assessment Project for the Southwest, this study is part of a larger effort to assess the vulnerability of natural and human systems to climate variability and change in the southwestern U.S. As importantly, this assessment seeks to fulfill the project’s larger mission of working directly with communities to improve their ability to respond adequately and appropriately to climatic events and climate change. The goal of this study is to demonstrate the utility of a rapid ethnographic approach for (1) conducting a community-level assessment of climate related vulnerability and (2) extending the findings to other assessments.

Tribes have a direct government-to-government relationship with the U.S. government wherein no decisions about their lands and people are made without their consent. In Arizona, for example, American Indian reservations occupy nearly 30 percent of the land. Native Americans have a legal and moral claim to significant quantities of water as well. Because of their special legal standing in the United States, tribes are not just another group of stakeholders to be considered in the research and policy process. The purpose of this paper is to provide a legal and political background for interactions between the United States and tribal governments and provide models for those interactions, with special attention to research and outreach.

This paper summarizes the current state of knowledge concerning the climate of the Southwest. Low annual precipitation, clear skies, and year-round warm weather over much of the Southwest are due in large part to a quasi-permanent subtropical high-pressure ridge over the region. However, the Southwest is located between the mid-latitude and subtropical atmospheric circulation regimes, and this positioning relative to shifts in these regimes is the fundamental reason for the region's climatic variability. El Niño, which is an increase in sea surface temperature of the eastern equatorial Pacific Ocean with an associated shift of the active center of atmospheric convection from the western to the central equatorial Pacific, has a well developed teleconnection with the Southwest, usually resulting in wet winters. La Niña, the opposite oceanic case of El Niño, usually results in dry winters for the Southwest. Another important oceanic influence on winter climate of the Southwest is a feature called the Pacific Decadal Oscillation, which has been defined as temporal variation in sea surface temperatures for most of the Northern Pacific Ocean. The major feature that sets climate of the Southwest apart from the rest of the United States is the North American monsoon, which, in the US, is most noticeable in Arizona and New Mexico. Up to 50% of the annual rainfall of Arizona and New Mexico occurs as monsoonal storms from July through September.