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  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 1978
    In:  Deep Sea Research Vol. 25, No. 1 ( 1978-01), p. 1-14
    In: Deep Sea Research, Elsevier BV, Vol. 25, No. 1 ( 1978-01), p. 1-14
    Type of Medium: Online Resource
    ISSN: 0146-6291
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1978
    detail.hit.zdb_id: 2196420-8
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  • 2
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1976
    In:  Journal of Fluid Mechanics Vol. 78, No. 1 ( 1976-11-05), p. 129-154
    In: Journal of Fluid Mechanics, Cambridge University Press (CUP), Vol. 78, No. 1 ( 1976-11-05), p. 129-154
    Abstract: In a turbulent two-dimensional flow enstrophy systematically cascades to very small scales, at which it is dissipated. The kinetic energy, on the other hand, remains at large scales and the total kinetic energy is constant. Above random topography an initially turbulent flow tends to a steady state with streamlines parallel to contours of constant depth, anticyclonic around a bump. A numerical experiment verifies this prediction. In a closed basin on a beta-plane the solution with minimum enstrophy implies a westward flow in the interior, returning in narrow boundary layers to the north and south. This result is interpreted using a parameterization of the effects of the eddies on the large-scale flow. The numerical solution is in qualitative agreement, but corresponds to a minimum of a more complex measure of the total enstrophy than the usual quadratic integral.
    Type of Medium: Online Resource
    ISSN: 0022-1120 , 1469-7645
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1976
    detail.hit.zdb_id: 1472346-3
    detail.hit.zdb_id: 218334-1
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1980
    In:  Reviews of Geophysics Vol. 18, No. 4 ( 1980-11), p. 789-812
    In: Reviews of Geophysics, American Geophysical Union (AGU), Vol. 18, No. 4 ( 1980-11), p. 789-812
    Abstract: A general approach is presented for estimating statistics of a random process from a finite data set from an irregularly spaced array of measurement locations. Particular attention is focused upon estimation of the spectrum under circumstances where it is smooth (i.e., broadband). A procedure is proposed based upon the technique of optimal linear estimation or generalized least squares fits in order to estimate coefficients of spectral features of interest to the investigator. Selection of which features are appropriate for estimation from a given array and set of measurements is made within the formalism of Bayesian statistical inference. The converse problem is also addressed: given a set of spectral features and a fixed number of possible measurements, which configuration of measurement locations will yield the most information about the amplitudes of those features? Finally, an assessment is made of the efficiency (i.e., the bias and accuracy) of various previously proposed methods of spectral estimation from irregular arrays.
    Type of Medium: Online Resource
    ISSN: 8755-1209 , 1944-9208
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1980
    detail.hit.zdb_id: 2035391-1
    detail.hit.zdb_id: 209852-0
    detail.hit.zdb_id: 209853-2
    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    Wiley ; 1975
    In:  Quarterly Journal of the Royal Meteorological Society Vol. 101, No. 430 ( 1975-10), p. 705-721
    In: Quarterly Journal of the Royal Meteorological Society, Wiley, Vol. 101, No. 430 ( 1975-10), p. 705-721
    Type of Medium: Online Resource
    ISSN: 0035-9009 , 1477-870X
    URL: Issue
    RVK:
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1975
    detail.hit.zdb_id: 3142-2
    detail.hit.zdb_id: 2089168-4
    SSG: 14
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  • 5
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1975
    In:  Journal of Fluid Mechanics Vol. 68, No. 02 ( 1975-3), p. 209-
    In: Journal of Fluid Mechanics, Cambridge University Press (CUP), Vol. 68, No. 02 ( 1975-3), p. 209-
    Type of Medium: Online Resource
    ISSN: 0022-1120 , 1469-7645
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1975
    detail.hit.zdb_id: 1472346-3
    detail.hit.zdb_id: 218334-1
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1993
    In:  Journal of Geophysical Research: Atmospheres Vol. 98, No. D9 ( 1993-09-20), p. 16669-16688
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 98, No. D9 ( 1993-09-20), p. 16669-16688
    Abstract: This paper presents an analysis of upper tropospheric relative humidity and clouds determined from geostationary satellite observations of the upwelling infrared radiation. The 6.7‐μm channel is located near the center of a strong water vapor absorption band and under clear sky conditions is primarily sensitive to the relative humidity averaged over a depth of atmosphere extending from 200 to 500 mbar. Estimates of the clear sky radiance at 6.7‐μm are obtained by utilizing the local spatial structure of the radiance field at 11‐μm and the correlation between 11‐μm and 6.7‐μm, to discriminate between clear and cloudy pixels. This approach is demonstrated to be more reliable than cloud clearance based solely upon the local spatial structure of the 6.7‐μm channel alone and provides estimates of the clear sky 6.7‐μm brightness temperature for areas 2° × 2° of latitude and longitude which are repeatable from successive images 30 min apart to within approximately 1 K. To facilitate the interpretation of the clear sky brightness temperatures, a simplified model of the radiative transfer at 6.7‐μm is presented. This model, based upon a set of irregularly spaced, strongly absorbing, pressure‐broadened lines, demonstrates that accurate to within approximately 1 K or 10% of the actual relative humidity, the brightness temperature at 6.7‐μm is proportional to the natural logarithm of the appropriate vertical average of the relative humidity divided by the cosine of the viewing zenith angle. Estimates of upper tropospheric water vapor inferred in this way from GOES E observations are presented for July 1987. The geographic distribution reflects many well‐known features of the large‐scale atmospheric circulation. A clear dependence of the greenhouse effect of upper tropospheric water vapor upon the large‐scale dynamics is also demonstrated. Finally, the observed relationship between the upper tropospheric relative humidity and the occurrence of upper tropospheric cloud cover is presented and its implications for the parameterization of clouds in general circulation models are discussed.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1993
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    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    Elsevier BV ; 1976
    In:  Deep Sea Research and Oceanographic Abstracts Vol. 23, No. 7 ( 1976-07), p. 559-582
    In: Deep Sea Research and Oceanographic Abstracts, Elsevier BV, Vol. 23, No. 7 ( 1976-07), p. 559-582
    Type of Medium: Online Resource
    ISSN: 0011-7471
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1976
    detail.hit.zdb_id: 2196421-X
    detail.hit.zdb_id: 426538-5
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  • 8
    Online Resource
    Online Resource
    American Meteorological Society ; 1977
    In:  Bulletin of the American Meteorological Society Vol. 58, No. 3 ( 1977-03), p. 230-232
    In: Bulletin of the American Meteorological Society, American Meteorological Society, Vol. 58, No. 3 ( 1977-03), p. 230-232
    Type of Medium: Online Resource
    ISSN: 0003-0007 , 1520-0477
    Language: English
    Publisher: American Meteorological Society
    Publication Date: 1977
    detail.hit.zdb_id: 2029396-3
    detail.hit.zdb_id: 419957-1
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1994
    In:  Journal of Geophysical Research: Atmospheres Vol. 99, No. D1 ( 1994-01-20), p. 1187-1210
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 99, No. D1 ( 1994-01-20), p. 1187-1210
    Abstract: This paper presents a comparison of the water vapor distribution obtained from two general circulation models, the European Centre for Medium‐Range Weather Forecasts (ECMWF) model and the National Center for Atmospheric Reseach (NCAR) Community Climate Model (CCM), with satellite observations of total precipitable water (TPW) from SSM/I and upper tropospheric relative humidity (UTH) from GOES. Overall, both models are successful in capturing the primary features of the observed water vapor distribution and its seasonal variation. For the ECMWF model, however, a systematic moist bias in TPW is noted over well‐known stratocumulus regions in the eastern subtropical oceans. Comparison with radiosonde profiles suggests that this problem is attributable to difficulties in modeling the shallowness of the boundary layer and large vertical water vapor gradients which characterize these regions. In comparison, the CCM is more successful in capturing the low values of TPW in the stratocumulus regions, although it tends to exhibit a dry bias over the eastern half of the subtropical oceans and a corresponding moist bias in the western half. The CCM also significantly overestimates the daily variability of the moisture fields in convective regions, suggesting a problem in simulating the temporal nature of moisture transport by deep convection. Comparison of the monthly mean UTH distribution indicates generally larger discrepancies than were noted for TPW owing to the greater influence of large‐scale dynamical processes in determining the distribution of UTH. In particular, the ECMWF model exhibits a distinct dry bias along the ITCZ and a moist bias over the subtropical descending branches of the Hadley cell, suggesting an underprediction in the strength of the Hadley circulation. The CCM, on the other hand, demonstrates greater discrepancies in UTH than are observed for the ECMWF model, but none that are as clearly correlated with well‐known features of the large‐scale circulation.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1994
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 10
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1996
    In:  Journal of Geophysical Research: Atmospheres Vol. 101, No. D5 ( 1996-04-27), p. 9333-9343
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 101, No. D5 ( 1996-04-27), p. 9333-9343
    Abstract: This study presents an analytical expression, derived from radiative theory, for relating water vapor radiances to layer‐average relative humidities. This “radiance‐to‐humidity transformation” provides a simple, yet reliable, means of interpreting satellite observations of the upwelling radiation in the 6.3‐μm water vapor absorption band in terms of a more familiar water vapor quantity. Despite its simplicity, when compared to detailed radiative transfer calculations of the upper (6.7 μm) tropospheric water vapor radiance, the transformation is demonstrated to be accurate to within ∼1 K. Similar levels of accuracy are found when the transformation is compared to detailed calculations of the middle (7.3 μm) and lower (8.3 μm) tropospheric water vapor radiance, provided that the emission from the underlying surface is taken into account. On the basis of these results, the radiance‐to‐humidity transformation is used to interpret TIROS operational vertical sounder observed water vapor radiances in terms of the relative humidity averaged over deep layers of the upper, middle, and lower troposphere. We then present near‐global maps of the geographic distribution and climatological variations of upper, middle, and lower‐tropospheric humidity for the period 1981–1991. These maps clearly depict the role of the large‐scale circulation in regulating the location and temporal variation of tropospheric water vapor.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1996
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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