The Origins of the Transgender Phenomenon: The Challenge and Opportunity for Training Lawyers, Judges and Policy Makers in the Historicity of Alfred Kinsey’s Pansexual Worldview

How has the country gone from a “firm reliance on the protection of Divine Providence” to where defining marriage as the union of one man and one woman is condemned as constitutionally irrational,and where the use of sex-separate private spaces by biological sex is subject to federal discrimination lawsuits?The answer can be traced to 1948 when Dr. Alfred C. Kinsey launched what was marketed then--and now--as the first “scientific” study of human sexuality.Indeed, Chief Judge of the Seventh Circuit Court of Appeals, Richard Posner extols Kinsey’s study as the “high-water mark of descriptive sexology.”Influential law professors such as Columbia University’s Herbert Wechslerand Yale University’s William Eskridge have ensured that Kinsey’s world shaking reports on male and female sexuality are entrenched as authoritative scientific research in legal scholarship and mainstream cultural institutions. Yet, Judge Posner, Professors Wechsler and Eskridge and the hundreds of other scholars who have relied upon this alleged “sex science” continue to cover up the facts: Kinsey’s claims are wholly fraudulent despite having ushered in the “sexual revolution” of the 1960s and 1970s. His fame was built on lies, and the massive criminal sexual abuse of children, significantly more damaging than the cover up of child sexual abuse by the Catholic Church and graphically apparent to anyone who reads Chapter Five of his report

Legal Responses to Genocide and Other Massive Violations of Human Rights

The international community could halt the proliferation of genocides by arresting them before, or at least while they are happening, by any means necessary. Instead, the focus is on actions after the fact

Institutions and Practices for Restoring and Maintaining Public Order

In the wake of the atrocities committed in Cambodia, southern Sudan, the former Yugoslavia, Rwanda and Haiti, many in the international community have called for the creation of ad hoc or standing international criminal courts to deal with some types of international delicts. Courts are indispensable institutions in many domestic criminal and civil systems, and any polity, no matter how structured, must have arrangements, of varying degrees of institutionalization, to apply the law to concrete cases. But lest we fall victim to a judicial romanticism in which we imagine that merely by creating entities we call courts we have solved major problems, we should review the fundamental goals that institutions designed to protect public order seek to fulfill. Goal clarification is especially important when our passions are engaged, as indeed they should be, upon encountering atrocities such as those of Rwanda. Indignation can be a powerful and productive source of political energy, but only if we tap it to stimulate the design of institutions that protect, restore, and improve public order

Situating the Next Generation of Impact Measurement and Evaluation for Impact Investing

In taking stock of the landscape, this paper promotes a convergence of methods, building from both the impact investment and evaluation fields.The commitment of impact investors to strengthen the process of generating evidence for their social returns alongside the evidence for financial returns is a veritable game changer. But social change is a complex business and good intentions do not necessarily translate into verifiable impact.As the public sector, bilaterals, and multilaterals increasingly partner with impact investors in achieving collective impact goals, the need for strong evidence about impact becomes even more compelling. The time has come to develop new mindsets and approaches that can be widely shared and employed in ways that will advance the frontier for impact measurement and evaluation of impact investing. Each of the menu options presented in this paper can contribute to building evidence about impact. The next generation of measurement will be stronger if the full range of options comes into play and the more evaluative approaches become commonplace as means for developing evidence and testing assumptions about the processes of change from a stakeholder perspective– with a view toward context and systems.Creating and sharing evidence about impact is a key lever for contributing to greater impact, demonstrating additionality, and for building confidence among potential investors, partners and observers in this emergent industry on its path to maturation. Further, the range of measurement options offers opportunities to choose appropriate approaches that will allow data to contribute to impact management– to improve on the business model of ventures and to improve services and systems that improve conditions for people and households living in poverty.

A Handbook of Data Collection Tools: Companion to "A Guide to Measuring Advocacy and Policy"

This handbook of data collection tools is intended to serve as a companion to A Guide to Measuring Advocacy and Policy. Organizational Research Services (ORS) developed this guide on behalf of the Annie E. Casey Foundation to support efforts to develop and implement an evaluation of advocacy and policy work. The companion handbook is dedicated to providing examples of practical tools and processes for collecting useful information from policy and advocacy efforts. Included within this handbook are a legislative process tracking log, a meeting observation checklist, a policy brief stakeholder survey, a policy tracking analysis tool, and a policy tracking form.This best practice provides an approach to measure advocacy and policy change efforts, starting with a theory of change, identifying outcome categories, and selecting practical approaches to measurement

Changes in the Greenland Ice Sheet of the Southeastern Maniitsoq Coast from 1994-2004 and 2009-2019

Remote sensing mechanisms through the use of technology like the Landsat 5-7 Land Manager satellites are commonly used in conjunction with multispectral methods such as unsupervised classification to record and analyze changes in snow and ice over time in areas such as the Greenland Ice Sheet (GrIS). Unsupervised classification is a method of identifying, grouping, and labeling features in an image according to their spectral values and is therefore a good method of classifying snow and ice in areas such as Greenland. The goal of unsupervised classifications is to assign pixels into potentially meaningful subsurface classes based on similarities of geophysical responses, in order to create a final product that displays an accurate class map of the land cover of the area (Kvamme, 2019). Within the southwestern region of Greenland is the town Maniitsoq along the (GrIS) that is surrounded by natural canal-like channels and located in the Qeqqata municipality. The southwestern Maniitsoq Greenland territory lies within the northernmost area south of the Arctic Circle and contains big, long, and deep glaciers. Temperatures in southern Greenland do not exceed 20 °C within the summer months of June, July, or August. Greenland is warmest and driest on land closest to the ice sheet during these summer months (Topas Travel, 2019). The location of our study area, the southwestern region of Greenland near Maniitsoq, was captured with Landsat imagery. The ice land cover was classified into three different sectional groups: changed snow/ice, unchanged snow/ice, and other. The research question of this project is as follows: how have the Greenland Ice Sheet glaciers along the eastern coast and inland Greenland changed from June through August of 1994-2004 and 2009-2019

Shock Wave Measurements in Cloud Cavitation

One of the most destructive (and noisy) forms of cavitation is that referred to as "cloud cavitation" because it involves a large collection of bubbles which behave as a coherent whole. The present paper presents the results of an experimental study of the processes of collapse of a cavitation bubble cloud, specifically that generated by an oscillating hydrofoil in a water tunnel. Measurements of the far-field noise show that this is comprised of substantial pulses radiated from the cloud at the moment of collapse. Also, transducers within the cavitation zone encounter very large pressure pulses (or shock waves) with amplitudes of the order of tens of atmospheres and typical durations of the order of tenths of a millisecond. These shock waves appear to be responsible for the enhanced noise and damage potential which results from that phenomenon

Pressure Pulses Generated by Cloud Cavitation

This paper describes an experimental investigation of the large unsteady and impulsive pressures which are experienced on the suction surface of both an oscillating and static hydrofoil as a result of cloud cavitation. The present experiments used piezo-electric transducers to measure unsteady pressures at four locations along the chord of the foil and at two locations along the walls of the tunnel test section. These transducers measured very large positive pressure pulses with amplitudes of the order of tens of atmospheres and with durations of the order of tenths of milliseconds. Two distinct types of pressure pulse were identified. "Local" pulses occurred at a single transducer location and were randomly distributed in position and time; several local impulses could be recorded by each transducer during an oscillation cycle. On the other hand, "global" impulses were registered by all the transducers almost simultaneously. Correlation of the transducer output with high speed movies of the cavitation revealed that they were produced by a large scale collapse of the bubble cloud. The location of the global impulses relative to the foil oscillation was quite repeatable and produced substantial far-field noise. The high speed movies also showed that the local impulses were caused both by crescent-shaped regions of low void fraction and by small bubbly structures. These regions appeared to be bounded by bubbly shock waves which were associated with the large pressure pulses. The paper also quantifies the effect of reduced frequency, cavitation number and tunnel velocity on the strength of the pressure pulses by presenting the acoustic impulse for a range of flow conditions. The reduced frequency is an important parameter in the determination of the total impulse level and the local and global pulse distribution. Large impulses are present on the foil surface even at cavitation numbers which do not result in large levels of acoustic radiation or global impulse. The total impulse increases with increasing tunnel velocity