Legislative Actions on Overtime Pay and Collective Bargaining and their Implications for Farm Employers in New York State, 2009-2010
Agricultural workers in most states are exempt from some labor law provisions that apply to employees in most other workplaces. In New York State agricultural labor advocates and farmers have battled politically over this issue for more than four decades. Two of the most contentious issues are collective bargaining and overtime pay. Currently laws for most other workers grant rights to employees who engage in union organizing activities. In addition, most employers are required to pay an overtime rate of time and one half for hours worked over 40 per week. In New York, labor advocates would like to see both of these exemptions for agriculture removed. Eleven states in the United States have laws that protect agricultural workers who wish to engage in collective bargaining and union organizing activities. In addition, four states have overtime pay provisions for agricultural workers. Introduced in the New York State Legislature in 2009, the Farmworkers Fair Labor Practices Act would have provided farmworkers with collective bargaining rights and overtime pay. It also contained other provisions viewed as having less impact on the agricultural industry. The proposal reignited a contentious debate and political standoff between farm business interests and the state’s labor advocates. The bill passed the Assembly on June 8, 2009. Leaders in the Senate had difficulty getting the bill to the Senate floor for a vote. Finally, as part of the 2010 state budget battle, Senator Pedro Espada, Senate Majority Leader, was successful in bringing about a vote. The legislation was defeated by a margin of three votes. Seldom has farmworker rights legislation gotten so close to passing both houses of the New York State Legislature with the prospect the Governor would sign it. The future prospects for overtime pay and collective bargaining rights for New York’s agricultural workers will continue to be dependent upon which political party controls the State Senate. The November 2010 elections resulted in the Republican Party recapturing the Senate majority making it unlikely that legislation similar to the Farmworkers Fair Labor Practices Act will be enacted in the near future. Both sides are extremely well organized and it appears possible this standoff could continue for many more years
Economic Analysis of the Financial Impact of the Grape Leafroll Virus (GLRV) in the Finger Lakes Region of New York
Economic analysis of the financial impact of the GLRV in the Finger Lakes region of NY 2 It is the Policy of Cornell University actively to support equality of educational and employment opportunity. No person shall be denied admission to any educational program or activity or be denied employment on the basis of any The University is committed to the maintenance of affirmative action programs which will assure the continuation of such equality of opportunity.
Imaging the Internal Structure of an Alpine Glacier via L-Band Airborne SAR Tomography
In this paper, we report results from the analysis of 3-D L-band airborne synthetic aperture radar (SAR) acquisitions acquired in March 2014 over the Mittelbergferner glacier, Austrian Alps, during the European Space Agency (ESA) campaign AlpTomoSAR. The campaign included coincident in situ measurements of snow and ice properties and ground-penetrating radar (GPR) data acquired at 600 and 200 MHz over a total length of 18 km. Radar data were acquired by repeatedly flying an L-band SAR along an oval racetrack at an altitude of about 1300 m over the glacier, such that two data stacks from opposite views are obtained. Data from all passes were coherently combined to achieve 3-D resolution capabilities, resulting in the generation of 3-D tomographic SAR (TomoSAR) cubes, where each voxel represents L-band radar reflectivity from a particular location in the 3-D space at a spatial resolution on the order of meters. TomoSAR cubes were finally corrected to account for wave propagation velocity into the ice, which was a necessary step to associate the observed features with their geometrical location, hence enabling a direct comparison to GPR data. The TomoSAR cubes show the complexity of the glacier subsurface scattering. Most areas are characterized by surface scattering in proximity of the ice surface, plus a complex pattern of in-depth volumetric scattering beneath and scattering at the ice/bedrock interface. Various subsurface features observed in GPR transects at 200 MHz clearly showed up in TomoSAR sections as well, particularly firn bodies, crevasses, layer transitions, and bedrock reflection down to 50 m below the ice surface.