The good otherwise satisfies any applicable regional value content (RVC) requirements specified in GN 33(b) and the good satisfies all other applicable requirements or.Each of the non-originating materials used in the production of the good undergoes an applicable change in tariff classification specified in GN 33(o) or.The good is produced entirely in the territory of one or more of the Parties and.The good is wholly obtained or produced entirely in the territory of the Parties (Republic of Korea, the United States or both).In general terms, under the KORUS a good is originating when: The HTSUS has been amended to include GN 33, both the general and specific rules of origin, definitions, and other related provisions. Section 202 of the KORUS Implementation Act specifies the rules of origin used to determine if a good “originates” under the Agreement. OriginationĪn originating good is one that meets the rules of origin set forth in GN 33 and all other requirements of the agreement. The text of the Agreement is posted on the website of the U.S.

Title 19, Code of Federal Regulations (CFR), was amended with the addition of Subpart R-United States-Korea Free Trade Agreement. The Agreement provides for the immediate or staged elimination of duties and barriers to bilateral trade in goods and services originating in the United States and/or Korea. Annex II of Publication 4308 amends the HTSUS to provide for immediate and staged tariff reductions. Annex I of Publication 4308 amends the Harmonized Tariff Schedule of the United States (HTSUS) with the addition of General Note 33 (GN 33) containing specific information regarding the KORUS and Subchapter XX to Chapter 99 providing for temporary tariff rate quotas (TRQs). The Proclamation incorporated, by reference, Publication 4308 of the United States International Trade Commission (USITC). Presidential Proclamation 8783, dated Maand published in the Federal Register on March 9, 2012, implements the U.S.-Korea Free Trade Agreement (KORUS) for goods entered, or withdrawn from warehouse for consumption, on or after March 15, 2012. The U.S.-Korea Free Trade Agreement Implementation Act (“the Act,” Pub. – Korea Free Trade Agreement (KORUS) Background Based on this physical model of the surface, the desert-reflected solar light’s polarization state at any wavelength in the whole solar spectra can be calculated with the ADRTM.U.S. The ratio of non-polarizer area to polarizer area and the angular distribution of the facet orientations are determined by fitting the modeled polarization states of light to the measurements at three polarized channels (490, 670, and 865 nm) by the Polarization and Anisotropy of Reflectances for Atmospheric Science instrument coupled with Observations from a Lidar (PARASOL).

Empirical models are adopted in obtaining the diffuse spectral reflectance of sands and the optical depth of the dust aerosols over the desert. The Adding–Doubling Radiative Transfer Model (ADRTM) is applied to integrate the atmospheric absorption and scattering in the system. The desert/bare land surface is assumed to be composed of two types of areas: fine sand grains with diffuse reflection (Lambertian non-polarizer) and quartz-rich sand particles with facets of various orientations (specular-reflection polarizer). In this study, an algorithm for deriving the spectral polarization state of solar light from the desert is reported. For correction of the measurement errors due to the light’s polarization, both the instrument’s dependence on the incident polarization state and the onorbit knowledge of the polarization state of light as a function of observed scene type, viewing geometry, and solar wavelength are required. To calibrate an Earth-observing sensor’s measurements with the highly accurate data from the CLARREO, errors in the measurements caused by the sensor’s sensitivity to the polarization state of light must be corrected. One of the major objectives of the Climate Absolute Radiance and Refractivity Observatory (CLARREO) is to conduct highly accurate spectral observations to provide an on-orbit inter-calibration standard for relevant Earthobserving sensors with various channels.

Korus spectra