Tion the decreasing solar altitude angle downward SC-19220 Description shortwave radiation decreased with
Tion the decreasing solar altitude angle downward shortwave radiation decreased with at SETORS fluctuated somewhat Theweakly, involving 300of downward shortwave radiation situated inside the northwesternThe dif (Z)-Semaxanib c-Met/HGFR annual variation W -2 and 400 W -2 . MAWORS is at QOMS was obvious. ference from the Tibetan Plateau, far inland, and is almost unaffected by the summer time monsoon. aspect involving the downward shortwave radiation in spring and summer season reached 200 At .that web page the downward shortwave radiation reached its maximumat SETORS fluctuated rel W -2 The annual variation of downward shortwave radiation in July.atively weakly, in between 300 W -2 and 400 W -2. MAWORS is situated within the northwest ern part in the Tibetan Plateau, far inland, and is virtually unaffected by the summer season mon quickly. At that web page the downward shortwave radiation reached its maximum in July.Water 2021, 13, x FOR PEER REVIEWWater 2021, 13, 3084 PEER Overview Water 2021, 13, x FOR9 ofof 26 9 9ofFigure 7. Annual variation of downward shortwave radiation (a) and diurnal variation of downward shortwave radiation (b) at each station.Annual variation of downward shortwave and diurnal variation of downward Figure 7. Annual variation of downward shortwave radiation (a) and diurnal variation of downward shortwave radiation The diurnal variation in downward shortwave radiation at every station (Figure 7b) (b) at every station.shows similar patterns at all stations. From eight:00, the downward shortwave radiation inThe diurnal variation in downward shortwave radiation at each and every station (Figure 7b) creased above zero, reaching a maximumshortwave radiation at each station returned7b) of 900 W -2 The diurnal variation all stations. From eight:00, the at about 14:00, and (Figure to shows similar patterns at in downward downward shortwave radiation adverse values at about 21:00. QOMS had the biggest diurnal range ofradiation inshows comparable patterns at all stations. Fromof 900 them-2 at about 14:00, and downward increased above zero, reaching a maximum 8:00, Wdownward shortwave returned to shortwave radiation reaching aW -2). SETORS had the at about 14:00, and returned to -2 smallest diurnal range (0 creased above zero, (0 to 950 maximum ofthe biggest diurnal range of downwardto 700 damaging values at around 21:00. QOMS had 900 W shortW -2). values at about 21:00. QOMS had the biggest diurnal variety of downward negative wave radiation (0 to 950 W -2 ). SETORS had the smallest diurnal variety (0 to 700 W -2 ). shortwave radiation (0 to 950 W -2). SETORS had the smallest diurnal range (0 to 700 three.2. Upward Shortwave Radiation Flux W -2). 3.2. Upward Shortwave Radiation Flux Upward shortwave radiation comes from the reflection of downward shortwave raUpward shortwave radiation comes in the reflection of downward shortwave three.2. Upward Shortwave Radiation Flux it it is mainly controlledby the downward shortwave diation in the surface. For that reason, is mainly controlled by the downward shortwave radiation from the surface. Hence, radiation and shortwave radiation comes fromvariations in upward shortwave radiation Upward the surface conditions. Diurnal the reflection of downward shortwave raradiation and also the surface circumstances. Diurnal variations in upward shortwave radiation (Figure from the surface.to these of downward shortwave radiation: upward shortwave (Figure 8b) have been related Thus, it is actually primarily controlled by the downward diation 8b) have been related to those of downward shortwave radiation: upward shortwave r.
