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The organization of spiral rainbands in a hurricane.Fung, Inez Yau-Sheung January 1977 (has links)
Thesis. 1977. Sc.D.--Massachusetts Institute of Technology. Dept. of Meteorology. / MICROFICHE COPY AVAILABLE IN ARCHIVES AND LINDGREN. / Vita. / Bibliography : leaves 136-139. / Sc.D.
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Numerical simulation of a long-lasting mesoscale convective line.Gordon, Neil David January 1978 (has links)
Thesis. 1978. Sc.D.--Massachusetts Institute of Technology. Dept. of Meteorology. / Microfiche copy available in Archives and Science. / Vita. / Bibliography : leaves 213-218. / Sc.D.
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The Eigensolutions of the balance equations over a sphere.Moura, Antônio Divino January 1975 (has links)
Thesis. 1975. Ph.D.--Massachusetts Institute of Technology. Dept. of Meteorology. / Vita. / Bibliography: leaves 168-170. / Ph.D.
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Predictability of an atmosphere with large-scale moisture patterns.Salstein, David Alan January 1976 (has links)
Thesis. 1976. Ph.D.--Massachusetts Institute of Technology. Dept. of Meteorology. / Microfiche copy available in Archives and Science. / Vita. / Bibliography: leaves 146-152. / Ph.D.
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Topographie et précipitation dans la vallée du Saint-Laurent.Fortin, J. P. (Jean Pierre). January 1965 (has links)
No description available.
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Comparative study and water budget of precipitation linesHaynes, Margaret Eugene January 1974 (has links)
No description available.
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Statistical studies of radar precipitation patterns.Zawadzki, Isztar Isaac January 1972 (has links)
No description available.
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An Analysis of Public Perception and Response to Hurricane SandyRice, Lindsay L. 16 April 2014 (has links)
Hurricane Sandy made landfall in Brigantine, New Jersey on October 29th, 2012. The storm impacted the coastal regions of New Jersey and New York, especially the heavily populated area of New York City. This research, which analyzes secondary data obtained from a telephone survey, investigates the public response of residents before, during and after Hurricane Sandy. The survey consisted of questions regarding what the residents expected concerning the threat of Hurricane Sandy, whether it matched what they experienced, where they got their information and how they made their decision to evacuate or not. The results from the survey were statistically analyzed in order to answer important research questions about public perception of Sandy's impacts. A Vulnerability Assessment of New York City, where some of Sandy's impacts were felt the most, was completed in order to understand why this area was so vulnerable. The concern level of various hurricane related hazards was analyzed and correlated to demographic variables to determine a relationship among the variables. A qualitative analysis was performed on the survey questions "Why did you evacuate?" and "Why did you not evacuate?" in order to determine themes in relation to people's reasons for evacuating or not evacuating. Finally, differences in how the public perceived Hurricane Sandy before and after the storm were analyzed and may be used for improving communication of the forecast to the public. Interdisciplinary research in this area is needed in order to better understand the public's need for appropriate warnings to ensure safety. Results show that residents were most concerned about wind damage and that they mainly used their television to obtain their information about the storm. Also, the most common reasons respondents reported for evacuating were because of the threat of possible impacts (storm surge, flooding, wind, rain and waves), the forecast called for bad conditions, or being told, recommended or convinced to leave. The main reasons reported by respondents for not evacuating are thinking that the impacts would not be bad in their area, feeling prepared or safe and thinking they could handle the impacts. This research can be used in the future for improving hurricane warning communication to the public.
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Occult cloudwater deposition to a forest in complex terrain : measurement and interpretationKowalski, Andrew S. 04 October 1996 (has links)
Occult deposition is the direct uptake of cloudwater by vegetation that comes into
physical contact with wind-driven cloud droplets. This can be a significant pathway for
hydrological and chemical fluxes from the atmosphere to some forests. Methods for
estimating cloudwater fluxes to forests are reviewed. Previous studies have neglected
the fact that cloudwater is not a conservative atmospheric quantity. This invalidates
traditional micrometeorological approaches for estimation of cloudwater fluxes to forests.
A theory is developed to predict the change in the cloudwater flux with height due to
condensation in the updrafts of orographic cloud, allowing estimation of surface uptake
via eddy correlation measurements while accounting for condensation.
The performances of three microphysical instruments are examined. From collocated
measurements, errors in cloud liquid water content are determined for a Particulate
Volume Monitor (PVM) and a Forward Scattering Spectrometer Probe (FSSP) to be less
than 0.01 g m⁻³ and 0.035 g m⁻³ respectively. Similarly, the error bounds for surface-normal
cloud liquid water fluxes are found to be 2 mg m⁻² s⁻¹ for the PVM and 3.5 mg
m⁻² s⁻¹ for the FSSP. Smaller errors are found to be associated with the uncertainty in the
direction of the flux relevant to surface uptake. The FSSP is seen to have larger errors
when droplet concentrations exceed 600 cm⁻³.
A vertical divergence is detected in the cloudwater flux; the downward flux
decreases with increasing distance from the surface, usually changing sign by 15 m above
ground. Five candidate processes are identified as possible explanations for this measured
flux divergence. A scale analysis shows that the liquid water source (condensation due
to pseudoadiabatic ascent) is largely responsible for the change in flux with height.
Accounting for the change in flux with height results in a near doubling of the estimated
surface flux relative to the flux measured at a height of 10 m in the surface layer for
this silver fir forest. This factor applies to chemical as well as liquid water fluxes. This
source of liquid water also is seen to be important in developing a simple model for
cloudwater deposition. / Graduation date: 1997
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Alberta hailstorms : a radar study and model.Chisholm, Alexander James January 1970 (has links)
No description available.
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