Is it ACT Yet? Real-World Examples of Evaluating the Degree of Implementation for Assertive Community Treatment

Despite growing interest in assessment of program implementation, little is known about the best way to evaluate whether a particular program has implemented the intended service to a level that is minimally acceptable to a funding source, such as a state mental health authority. Such is the case for assertive community treatment (ACT), an evidence-based practice being widely disseminated. Using an exploratory, actuarial approach to defining program standards, this study applies different statistical criteria for determining whether or not a program meets ACT standards using the 28-item Dartmouth Assertive Community Treatment Scale. The sample consists of 51 ACT programs, 25 intensive case management programs, and 11 brokered case management programs which were compared to identify levels of fidelity that discriminated between programs, but were still attainable by the majority of ACT programs. A grading system based on mean total score for a reduced set of 21 items appeared to be most attainable, but still discriminated ACT programs from other forms of case management. Implications for setting and evaluating ACT program standards are discussed

Northern peatland initiation lagged abrupt increases in deglacial atmospheric CH4

Peatlands are a key component of the global carbon cycle. Chronologies of peatland initiation are typically based on compiled basal peat radiocarbon (14C) dates and frequency histograms of binned calibrated age ranges. However, such compilations are problematic because poor quality 14C dates are commonly included and because frequency histograms of binned age ranges introduce chronological artefacts that bias the record of peatland initiation. Using a published compilation of 274 basal 14C dates from Alaska as a case study, we show that nearly half the 14C dates are inappropriate for reconstructing peatland initiation, and that the temporal structure of peatland initiation is sensitive to sampling biases and treatment of calibrated 14C dates. We present revised chronologies of peatland initiation for Alaska and the circumpolar Arctic based on summed probability distributions of calibrated 14C dates. These revised chronologies reveal that northern peatland initiation lagged abrupt increases in atmospheric CH4 concentration at the start of the Bølling–Allerød interstadial (Termination 1A) and the end of the Younger Dryas chronozone (Termination 1B), suggesting that northern peatlands were not the primary drivers of the rapid increases in atmospheric CH4. Our results demonstrate that subtle methodological changes in the synthesis of basal 14C ages lead to substantially different interpretations of temporal trends in peatland initiation, with direct implications for the role of peatlands in the global carbon cycle