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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
11

Meteorological investigation of ozone anomalies during the arctic boundary layer experiment (ABLE 3A)

Smarsh, David Anthony 08 1900 (has links)
No description available.
12

Environmental factors affecting net CO2 assimilation in Cladonia alpestris (L.) Rabh. in the subarctic

Carstairs, Anne Graham. January 1976 (has links)
No description available.
13

Marine bivalve molluscs of the Canadian arctic.

Lubinsky, Irene. January 1972 (has links)
No description available.
14

Sea ice in the Canadian Arctic Archipelago

Lindsay, D. G. (Donald Gordon) January 1968 (has links)
No description available.
15

An analysis of one year of surface layer meteorological data from the Arctic pack ice

Baumann, Richard James 17 July 1978 (has links)
The thesis describes the properties of surface wind and air temperature time series recorded at three locations on the pack ice of the Beaufort Sea. Time series consisting of sequential one-half hourly means were constructed for a period of approximately a year. A diurnal fluctuation in air temperature is found for the late summer, early fall and spring seasons only. Wind speed does not show a significant diurnal fluctuation for any season. There is very little seasonal variability in the wind speed while significant variation is present in the air temperature. The integrated wind speed spectrum (i. e. variance) is 80% less than the integrated sum of the wind component spectra indicating that for periods longer than a day, directional fluctuations contribute much more to the variance of the wind record than do speed fluctuations. Although the measurements only approach the microscale region, there seems to be no consistent indication of a microscale peak in the variance preserving representation of the wind speed spectrum. Time series of daily mean horizontal divergence and vertical component of vorticity for both the wind field and ice motion are examined. For a period of 355 days there is significant negative correlation (-0.65) between the wind divergence and wind vorticity series and significant positive correlation (0.65) between the wind vorticity and ice vorticity series. / Graduation date: 1979
16

An assessment of NOGAPS performance in Polar Forecasting from SHEBA data /

Lana, Aaron D. Unknown Date (has links) (PDF)
Thesis (M.S. in Meteorology and Physical Oceanography)--Naval Postgraduate School, 2004. / Thesis Advisor(s): Peter Guest. Includes bibliographical references (p. 63-64). Also available online.
17

Toward quantifying the impact of atmospheric forcing on Arctic sea ice variability using the NPS 1/12 degree pan-Arctic coupled ice-ocean model

Tseng, Hsien-Liang R. January 2010 (has links) (PDF)
Thesis (M.S. in Meteorology and M.S. in Physical Oceanorgraphy)--Naval Postgraduate School, March 2010. / Thesis Advisor(s): Maslowski, Wieslaw ; Stone, Rebecca E. "March 2010." Description based on title screen as viewed on April 26, 2010. Author(s) subject terms: Arctic Sea Ice, Sea Ice Extent, Sea Ice Thickness, Sea Ice Volume, Coupled Ice-Ocean Model, Partial Correlation Coefficient, Surface Air Temperature, Arctic Oscillation, Atmospheric Forcing, Oceanic Forcing. Includes bibliographical references (p.163-168). Also available in print.
18

Effects of Natural Disturbance on Arctic Stream Communities

Parker, Stephanie Megan January 2004 (has links) (PDF)
No description available.
19

Environmental factors affecting net CO2 assimilation in Cladonia alpestris (L.) Rabh. in the subarctic

Carstairs, Anne Graham. January 1976 (has links)
No description available.
20

Sea ice in the Canadian Arctic Archipelago

Lindsay, D. G. (Donald Gordon) January 1968 (has links)
No description available.

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