Diurnal

Results: 225



#Item
1WESTERN BIRDS Volume 42, Number 2, 2011 WINTER HABITAT ASSOCIATIONS OF DIURNAL RAPTORS IN CALIFORNIA’S CENTRAL VALLEY Edward R. Pandolfino, 5530 Delrose Court, Carmichael, California 95608;

WESTERN BIRDS Volume 42, Number 2, 2011 WINTER HABITAT ASSOCIATIONS OF DIURNAL RAPTORS IN CALIFORNIA’S CENTRAL VALLEY Edward R. Pandolfino, 5530 Delrose Court, Carmichael, California 95608;

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Source URL: www.carangeland.org

Language: English - Date: 2017-09-08 07:14:38
    2JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, D11206, doi:2005JD006515, 2006 Seasonal and diurnal variations of submicron organic aerosol in Tokyo observed using the Aerodyne aerosol mass spectrometer N. Takegawa,1

    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, D11206, doi:2005JD006515, 2006 Seasonal and diurnal variations of submicron organic aerosol in Tokyo observed using the Aerodyne aerosol mass spectrometer N. Takegawa,1

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    Source URL: www.asrc.cestm.albany.edu

    - Date: 2006-06-10 14:22:19
      33.2 Development of multiscale modeling capabilities within WRF: Validation on idealized cases and a diurnal cycle of the CWEX-13 field campaign. Muñoz-Esparza, Domingo, Branko Kosović, National Center for Atmospher

      3.2 Development of multiscale modeling capabilities within WRF: Validation on idealized cases and a diurnal cycle of the CWEX-13 field campaign. Muñoz-Esparza, Domingo, Branko Kosović, National Center for Atmospher

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      Source URL: www2.mmm.ucar.edu

      - Date: 2016-06-16 12:19:59
        4Diurnal and Seasonal Surface Temperature Variations: A Case Study in Baghdad Mustafa Naem, Robert Corner, and Ashraf Dewan Department of Spatial Sciences, Curtin University, WA, Australia; Emails:

        Diurnal and Seasonal Surface Temperature Variations: A Case Study in Baghdad Mustafa Naem, Robert Corner, and Ashraf Dewan Department of Spatial Sciences, Curtin University, WA, Australia; Emails:

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        Source URL: ceur-ws.org

        Language: English - Date: 2016-03-05 11:12:24
        5J. N. Am. Benthol. Soc., 2006, 25(3):583–595 Ó 2006 by The North American Benthological Society Effects of light on NO3 uptake in small forested streams: diurnal and day-to-day variations

        J. N. Am. Benthol. Soc., 2006, 25(3):583–595 Ó 2006 by The North American Benthological Society Effects of light on NO3 uptake in small forested streams: diurnal and day-to-day variations

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        Source URL: walkerbranch.ornl.gov

        Language: English - Date: 2010-02-10 14:40:09
        6On improved representation of the diurnal cycle over a semi-arid, metropolitan area Matei Georgescu, Mohamed Moustaoui, Alex Mahalov School of Mathematical and Statistical Sciences and Center for Environmental Fluid Dyna

        On improved representation of the diurnal cycle over a semi-arid, metropolitan area Matei Georgescu, Mohamed Moustaoui, Alex Mahalov School of Mathematical and Statistical Sciences and Center for Environmental Fluid Dyna

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        Source URL: www2.mmm.ucar.edu

        Language: English - Date: 2011-07-19 10:49:06
        7Atmospheric sciences / Meteorology / Physics / Heat transfer / Rudrasagar Lake / Tide / Temperature / Atmosphere of Earth / Climate / MEMO Model / Properties of water

        Modeling of diurnal profile of surface air temperature and surface dissolved oxygen of lake water Mihir Pal 1*, Nihar R. Samal 2, Malabika B. Roy 3 and Pankaj k. Roy4

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        Source URL: www.currentscience.ac.in

        Language: English - Date: 2016-07-05 01:26:04
        8Journal of Glaciology, Vol. 60, No. 224, 2014 doi: 2014JoG13J230Evidence for non-tidal diurnal velocity variations of Helheim Glacier, East Greenland

        Journal of Glaciology, Vol. 60, No. 224, 2014 doi: 2014JoG13J230Evidence for non-tidal diurnal velocity variations of Helheim Glacier, East Greenland

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        Source URL: www.haystack.edu

        Language: English - Date: 2014-12-17 07:55:07
        9Convective Boundary Layer be spun up (i.e., its turbulence intensity must increase from near zero to the current ML value) as entrainment incorporates it into the ML. Over a land surface experiencing a strong diurnal c

        Convective Boundary Layer be spun up (i.e., its turbulence intensity must increase from near zero to the current ML value) as entrainment incorporates it into the ML. Over a land surface experiencing a strong diurnal c

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        Source URL: climate-dynamics.org

        Language: English - Date: 2016-03-17 05:07:51