180,463 research outputs found
[Telegram from Mr. and Mrs. Richard Hickman to Odelia R. Staiti - October 5, 1933]
No full textTelegram from Mr. and Mrs. Richard Hickman to Odelia R. Staiti, offering sympathy regarding the recent passing of her husband, Henry T. Staiti
[Letter from Donald N. McKenzie to Pauline Vashti R. Hickman - October 13, 1918]
No full textLetter from Donald N. McKenzie to Pauline Vashti Hickman (née Reisner; "Mrs. Harry Hickman"), offering sympathy regarding the passing of Grover Staiti; text: "Dear Mrs. Hickman:- Please express to your sister and others of the family my sincere sympathy in their great bereavement. Sincerely, Donald N. McKenzie
[Telegram from E. D. Joost to Mr. and Mrs. Richard Hickman - October 5, 1933]
No full textTelegram from E. D. Joost, secretary on behalf of Odelia R. Staiti, to Mr. and Mrs. Richard Hickman of Saticoy or Duarte, California, informing them of the passing of Henry Staiti on Monday, October 2, 1933
[Telegram from E. D. Joost to Mr. and Mrs. Edgar Hickman - October 5, 1933]
No full textTelegram from E. D. Joost, secretary on behalf of Odelia R. Staiti, to Mr. and Mrs. Edgar Hickman of La Mesa, informing them of the passing of Henry Staiti on Monday, October 2, 1933
Tom R. Hickman
No full textTom R. Hickman, full body shot.https://mavmatrix.uta.edu/specialcollections_startelegram1950s/27307/thumbnail.jp
S2P3-R (v1.0): a framework for efficient regional modelling of physical and biological structures and processes in shelf seas
No full textAn established one-dimensional (1-D) model of Shelf Sea Physics and Primary Production (S2P3) is adapted for flexible use in selected regional settings over selected periods of time. This Regional adaptation of S2P3, the S2P3-R framework (v1.0), can be efficiently used to investigate physical and biological phenomena in shelf seas that are strongly controlled by vertical processes. These include spring blooms that follow the onset of stratification, tidal mixing fronts that seasonally develop at boundaries between mixed and stratified water, and sub-surface chlorophyll maxima that persist throughout summer. While not representing 3-D processes, S2P3-R reveals the horizontal variation of the key 1-D (vertical) processes. S2P3-R should therefore only be used in regions where horizontal processes – including mean flows, eddy fluxes and internal tides – are known to exert a weak influence in comparison with vertical processes. In such cases, S2P3-R may be used as a highly versatile research tool, alongside more complex and computationally expensive models. In undergraduate oceanography modules and research projects, the model serves as an effective practical tool for linking theory and field observations. Three different regional configurations of S2P3-R are described, illustrating a range of diagnostics, evaluated where practical with observations. The model can be forced with daily meteorological variables for any selected year in the reanalysis era (1948 onwards). Example simulations illustrate the considerable extent of synoptic-to-interannual variability in the physics and biology of shelf seas. In discussion, the present limitations of S2P3-R are emphasised, and future developments are outlined
Paul R. Olson et C. Addison Hickman. Pan American Economics
No full textGuillet Dominique. Paul R. Olson et C. Addison Hickman. Pan American Economics. In: Politique étrangère, n°3 - 1945 - 10ᵉannée. pp. 293-295
Mitigating the risk of HIV infection with opioid substitution treatment
No full textLinda R Gowing, Matthew Hickman & Louisa Degenhard
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