Norms for the Spanish version of the Eating Disorders Examination Questionnaire (S-EDE-Q)

Resumen tomado de la publicación

Normative scores of the Cambridge Cognitive Examination-Revised in healthy Spanish population

Resumen tomado de la publicaci??n

Examination of parent support groups for newly diagnosed hearing-impaired children, birth - 5 years

This paper examines support groups for parents of newly-diagnosed hearing-impaired children and presents an outline for an effective parent support group.

An examination of the appropriateness of the CID grammatical analysis of elicted language as an instrument to compare language acquisition in deaf children enrolled in cued speech vs. oral and signed english programs

This paper discusses a study to compare test results of the CID GAEL test among hearing impaired children who are enrolled in cued speech vs. oral vs. signed english programs.

An examination of cued speech as a tool for language, literacy, and bilingualism for children who are deaf or hard of hearing

This study examines the purpose and uses of Cued Speech, its benefits and limitations, and its effectiveness as a tool for language, literacy, and bilingualism.

Examination of Relationships between Clear-Sky Longwave Radiation and Aspects of the Atmospheric Hydrological Cycle in Climate Models, Reanalyses, and Observations

Relationships between clear-sky longwave radiation and aspects of the atmospheric hydrological cycle are quantified in models, reanalyses, and observations over the period 1980-2000. The robust sensitivity of clear-sky surface net longwave radiation (SNLc) to column-integrated water vapor (CWV) of 1-1.5 Wm(-2) mm(-1) combined with the positive relationship between CWV and surface temperature (T-s) explains substantial increases in clear-sky longwave radiative cooling of the atmosphere (Q(LWc)) to the surface over the period. Clear-sky outgoing longwave radiation (OLRc) is highly sensitive to changes in aerosol and greenhouse gas concentrations in addition to temperature and humidity. Over tropical ocean regions of mean descent, Q(LWc) increases with T-s at similar to 3.5-5.5 W m(-2) K-1 for reanalyses, estimates derived from satellite data, and models without volcanic forcing included. Increased Q(LWc) with warming across the tropical oceans helps to explain model ensemble mean increases in precipitation of 0.1-0.15 mm day(-1) K-1, which are primarily determined by ascent regions where precipitation increases at the rate expected from the Clausius-Clapeyron equation. The implications for future projections in the atmospheric hydrological cycle are discussed