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Data & statistics on Average ratio of heat flux components to net radiation – 3474 results

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Wind stress and heat flux statistics for LMG02-01A Leg 2. Heat flux components are: net heat flux–Qnet; shortwave radiation–Qsw; longwave radiation–Qlw; sensible heat flux–Qsen; and latent heat flux–Qlat. Units for wind stress are N m-2; those for heat flux are W m-2.

Wind stress and heat flux statistics for LMG02-01A Leg 2. Heat flux components are: net heat flux–Qnet; shortwave radiation–Qsw; longwave radiation–Qlw; sensible heat flux–Qsen; and latent heat ...

www.ccpo.odu.edu/Research/globec/main_cruises02/lmg0201a/LMG02-01A_Report.pdf

components are: net heat flux–Qnet; shortwave radiation–Qsw; longwave radiation–Qlw ...
The resulting net radiation flux was -31 W m-2, roughly comparable with the mean net heat ...
Table 5 gives simple statistics for the east (Tx) and north (Ty) wind stress and the heat flux components for Leg 2.

Jul 2002 | CCPO Graduate Programs
Original Url: http://www.ccpo.odu.edu/Research/globec/main_cruises02/lmg0201a/LMG02-01A_Report.pdf
Equation 3 states that the net TOA radiative flux is the sum of the net shortwave (SW) flux and the longwave (LW) flux. The net SFC energy flux (equation 4) also includes SW and LW radiative components, and additionally a non-radiative component associated with the turbulent exchange of latent heat (LH) and sensible heat (SH) between the surface and atmosphere. Equation 5 states that the total atmospheric ...

Equation 3 states that the net TOA radiative flux is the sum of the net shortwave (SW) flux and the longwave (LW) flux. The net SFC energy flux (equation 4) also includes SW and LW radiative ...

www.columbia.edu/~lmp/paps/previdi%2Bsmith%2Bpolvani-JCLIM-2012-revised.pdf

Fk + Fq + FΦ T g Equation 3 states that the net TOA radiative flux is the sum ...
radiative component associated with the turbulent exchange of latent heat (LH ...
where ∂E/∂t is the energy storage, FTOA:NET is the TOA net radiative energy

Jan 2013 | Columbia University in the City of New York
Original Url: http://www.columbia.edu/~lmp/paps/previdi%2Bsmith%2Bpolvani-JCLIM-2012-revised.pdf
Energy balance (W m-2)of each terrain type (June 2 1 to August 18). Q' is net radiation, C the latent heat flux, Q, the & sensible heat flux, Qc the soil heat flux, and P the Bowen ratio. Flux ratios and P are unitless
8 more results from this site ▶

Energy balance (W m-2)of each terrain type (June 2 1 to August 18). Q' is net radiation, C the latent heat flux, Q, the & sensible heat flux, Qc the soil heat flux, and P the Bowen ratio. Flux ratios ...

www.int-res.com/articles/cr/5/c005p031.pdf

is available to go into warming the atmosphere (QH). During the day, the sensible heat flux ...
flux allows more energy to be used for sensible heating of the air compared ...
from these wet surfaces. The smallest ground heat flux occurred in the sedge wetland

Nov 2006 | Inter Research »  – 8 more results from this site
Original Url: http://www.int-res.com/articles/cr/5/c005p031.pdf
Time series of (a) the modeled net surface radiation and the sum of the surface fluxes and (b) the component surface latent and sensible heat fluxes for the S1-100 simulations.
16 more results from this site ▶

Time series of (a) the modeled net surface radiation and the sum of the surface fluxes and (b) the component surface latent and sensible heat fluxes for the S1-100 simulations.

www.atmos.washington.edu/2008Q2/591A/Articles/Jiang_2.pdf

into its sensible and latent heat flux components. The mean Bowen ratio over the period 08:00 ...
to have higher latent heat fluxes than observed seasonally averaged values. Other sources ...
season and observations of the sensible heat flux [Fisch et al., 2004] show maximum

Dec 2005 | UW Dept of Atmospheric Sciences – 16 more results from this site
Original Url: http://www.atmos.washington.edu/2008Q2/591A/Articles/Jiang_2.pdf
Time-averaged surface heat flux components in (a) Box 1, (b) Box 2 and (c) Box 3 for each period, representing pre-Gustav (T1), Gustav (T2), post-Gustav (T3), Ike (T4) and post-Ike (T5) duration, respectively. Surface heat flux terms include incoming short wave radiation (QSWR), outgoing long wave radiation (QLWR), latent heat flux (QLAT), sensible heat flux (QSEN) and net surface heat flux (QSHF). ...

Time-averaged surface heat flux components in (a) Box 1, (b) Box 2 and (c) Box 3 for each period, representing pre-Gustav (T1), Gustav (T2), post-Gustav (T3), Ike (T4) and post-Ike (T5) duration, ...

omglnx6.meas.ncsu.edu/hyun/literature/DYNAT-S-10-00088.pdf

(a) (b) (c)

Dec 2010 | omglnx6.meas.ncsu.edu
Original Url: http://omglnx6.meas.ncsu.edu/hyun/literature/DYNAT-S-10-00088.pdf
Seasonal variations of long-wave radiation, sensible and latent heat fluxes at the station in Harima-Nada, spatially averaged short-wave radiation over whole model domain and the sum of four components of heat flux, i.e., net heat flux.

Seasonal variations of long-wave radiation, sensible and latent heat fluxes at the station in Harima-Nada, spatially averaged short-wave radiation over whole model domain and the sum of four ...

www.ehime-u.ac.jp/~cmes/xguo/paper/Chang2009JO.pdf

where QO is the surface heat flux. The monthly mean QO of is computed ...
variation of spatially averaged QO (i.e., long-wave radiation, sensible and latent fluxes) and short-wave radiation Qs. Surface salinity flux, W s is calculated

Oct 2009 | 愛媛大学
Original Url: http://www.ehime-u.ac.jp/~cmes/xguo/paper/Chang2009JO.pdf
Time series of daily – averaged flux components: solar radiative flux (dashed blue), net infrared radiative flux (cyan x), sensible heat flux (green solid), and latent heat flux (red dots).

Time series of daily – averaged flux components: solar radiative flux (dashed blue), net infrared radiative flux (cyan x), sensible heat flux (green solid), and latent heat flux (red dots).

uop.whoi.edu/projects/stratus/docs/Stratus2Cruise.pdf

Apr 2002 | UOP : Upper Ocean Processes Group : WHOI
Original Url: http://uop.whoi.edu/projects/stratus/docs/Stratus2Cruise.pdf
Net radiation (R,), sensible (H) and latent (LE) heat fluxes, and soil heat flux (G) as measured by eddy correlation technique in the sand-dominated portion of the Owens Lake playa.

Net radiation (R, ), sensible (H) and latent (LE) heat fluxes, and soil heat flux (G) as measured by eddy correlation technique in the sand-dominated portion of the Owens Lake playa.

wolfweb.unr.edu/homepage/tylers/pdfpapers/journofhydro/tyleretal1996jofH.pdf

~" IT ~ -~, ~ ~ 3L~LI ~rl~l ~ _ ' m ~rr'rl~rj -J, Or) I Julian Days, 1993 Net Radiation Sensible Heat Flux o Soil Heat Flux • LatentHeat Flux ...
01 mm day -~) in comparison with the average daily evaporation rate. Bowen ratio measurements of evaporation were conducted from 20 to 24 June 1993. Negative Bowen ratios ...
Bowen ratio measurements of evaporation on playa surfaces, the technique, combined

Jan 1993 | University of Nevada, Reno - Wolfweb Websites
Original Url: http://wolfweb.unr.edu/homepage/tylers/pdfpapers/journofhydro/tyleretal1996jofH.pdf
Surface energy-balance components estimated in conjunction with energy-balance Bowen ratio measurements and summed over 24-hour and daytime periods for a dry prairie site on June 13, 1990, and for a marsh site on June 16, 1990 [MJ/m2, megajoules per square meter; Rn, net radiation; G, subsurface heat flux; H, sensible heat flux; LE, latent heat flux]

Surface energy-balance components estimated in conjunction with energy-balance Bowen ratio measurements and summed over 24-hour and daytime periods for a dry prairie site on June 13, 1990, and for a ...

fl.water.usgs.gov/PDF_files/wsp2430_bidlake.pdf

megajoules per square meter; Rn, net radiation; G, subsurface heat flux; H, sensible heat flux; LE, latent heat flux] Rn G H LE Measurement period Bowen ratio (MJ/m2) (MJ/m2 ...
was that subsurface heat flux was small in comparison to the remaining fluxes. Measured subsurface heat flux was less than 3 percent of the latent heat flux during 24 hours. At the dry prairie site, daytime subsurface heat flux was approximately 18 percent ...
hour ......... Daytime ........ 1Subsurface heat flux at the marsh site

Jan 1990 | Florida Integrated Science Center - Water Resources
Original Url: http://fl.water.usgs.gov/PDF_files/wsp2430_bidlake.pdf
The relationship between daily net radiation and latent heat flux at Zotino (A) and Fyodorovskoye (B) for 1998 (closed circles), 1999 (closed triangles) and 2000 (grey circles). Data before snowmelt or at days after snowmelt when average temperatures <5 °C are indicated as open circles. The lines are linear regressions through the data where 1998 = dashed line, 1999 = straight line, 2000 = dotted ...

The relationship between daily net radiation and latent heat flux at Zotino (A) and Fyodorovskoye (B) for 1998 (closed circles), 1999 (closed triangles) and 2000 (grey circles). Data before snowmelt ...

forest.akadem.ru/Articles/02/tchebakova_3.pdf

of all components of the energy balance, particularly of soil heat flux, are difficult to perform in wetlands. We therefore do not know the ratio of (H + λE)/Ra for the two study sites and have not adjusted the fluxes for closure, with the consequence

Jan 2000 | Институт Леса им. В.Н.Сукачёва
Original Url: http://forest.akadem.ru/Articles/02/tchebakova_3.pdf
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