Research Article
Annual Observations of Climatic Impacts in the Songhua River Basin, China
Table 2
Daily averages of the seasonal heat flux gains (+) and losses (−). The values in bold indicate the percentage contribution of each flux component.
| | Seasons | Net radiation flux | Latent heat flux | Sensible heat flux | Conductive heat flux to river | | + | − | + | − | + | − | + | − |
| | Spring (W/m2) | 314.88 | 26.92 | 9.82 | 234.40 | 15.99 | 8.69 | 25.41 | 96.09 | | Percentage contribution (%) | 86.01 | 7.35 | 2.68 | 64.03 | 4.37 | 2.37 | 6.94 | 26.25 |
| | Summer (W/m2) | 146.58 | 12.61 | 6.1 | 133.39 | 0.62 | 7.77 | 15.45 | 14.98 | | Percentage contribution (%) | 86.87 | 7.47 | 3.61 | 79.04 | 0.37 | 4.61 | 9.15 | 8.88 |
| | Autumn (W/m2) | 62.80 | 74.2 | 31.02 | 56.71 | 3.60 | 16.37 | 62.46 | 12.61 | | Percentage contribution (%) | 39.28 | 46.41 | 19.40 | 35.47 | 2.25 | 10.24 | 39.07 | 7.89 |
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