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2![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 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](https://www.pdfsearch.io/img/b9cfd086151966471b0bdbf345d57f51.jpg) | Add to Reading ListSource URL: www.asrc.cestm.albany.edu- Date: 2006-06-10 14:22:19
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3![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 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](https://www.pdfsearch.io/img/7d9b68ebc92facd967f507606d4be5a4.jpg) | Add to Reading ListSource URL: www2.mmm.ucar.edu- Date: 2016-06-16 12:19:59
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4![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: 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:](https://www.pdfsearch.io/img/fe885b6deb703e324fd6877dac27af15.jpg) | Add to Reading ListSource URL: ceur-ws.orgLanguage: English - Date: 2016-03-05 11:12:24
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5![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 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](https://www.pdfsearch.io/img/88f2d00bfcc9ddd4eee1a92cae64d90a.jpg) | Add to Reading ListSource URL: walkerbranch.ornl.govLanguage: English - Date: 2010-02-10 14:40:09
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6![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 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](https://www.pdfsearch.io/img/965f053253007ddebec9eddc318fec65.jpg) | Add to Reading ListSource URL: www2.mmm.ucar.eduLanguage: English - Date: 2011-07-19 10:49:06
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7![Atmospheric sciences / Meteorology / Physics / Heat transfer / Rudrasagar Lake / Tide / Temperature / Atmosphere of Earth / Climate / MEMO Model / Properties of water Atmospheric sciences / Meteorology / Physics / Heat transfer / Rudrasagar Lake / Tide / Temperature / Atmosphere of Earth / Climate / MEMO Model / Properties of water](/pdf-icon.png) | Add to Reading ListSource URL: www.currentscience.ac.inLanguage: English - Date: 2016-07-05 01:26:04
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8![Journal 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](https://www.pdfsearch.io/img/3cae1de77875bed2cc18682cf9ddb5cc.jpg) | Add to Reading ListSource URL: www.haystack.eduLanguage: English - Date: 2014-12-17 07:55:07
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9![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 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](https://www.pdfsearch.io/img/b5029d077fcecab7cdc0791fe033bee5.jpg) | Add to Reading ListSource URL: climate-dynamics.orgLanguage: English - Date: 2016-03-17 05:07:51
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