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عمران::
در مثال 3 به شکل کامل مدل تبخیری آمستردام ترجمه شود ، در باقی موارد از حروف اختصاری استفاده شود.
In GLEAM_v3.0b, the root zone depth depends on the respective land cover type and is 0-250 cm for tall vegetation, 0-100 cm for low vegetation, and 0-10 cm for bare soil (Martens et al. 2017).
ERA MERRA-2 COMB Latent heat flux ERA-Interim/Land MERRA-2 GLEAM_v3.0b Sensible heat flux ERA-Interim/Land MERRA-2 - Net radiation ERA-Interim/Land MERRA-2 CERES Soil moisture (root zone) ERA-Interim/Land (0-100 cm) MERRA-2 (0-100 cm) GLEAM_v3.0b (root zone) 2-m air temperature (daily maximum) ERA-Interim MERRA-2 Berkeley Earth Analyzed time period 1980-2009 1980-2009 2003-13
The dataset com- bination (hereinafter referred to as COMB) uses the Global Land Evaporation Amsterdam Model (GLEAM_v3.0b; Miralles et al. 2011; Martens et al. 2017) for latent heat flux and soil moisture, CERES for net radiation (Wielicki et al. 1996), and Berkeley Earth surface temperature for daily maximum 2-m air tem- perature (Rohde et al. 2013a,b).
Soil moisture in GLEAM_v3.0b is calculated by combining satellite measurements of soil moisture in the top layer with a simple empirical drainage algorithm to estimate the water content in the complete root zone.
We want to highlight here that the GLEAM_v3.0b data, while relying on various obser- vations, do not include direct measurements of root zone soil moisture or latent heat flux, the quantities of rele- vance to this study.
واژگان شبکه مترجمین ایران