Abstract
The characteristics of net radiation (R n) (0.3–10 µm) in Lhasa and Haibei in the Tibetan Plateau were analyzed based on long-term in-situ measurements of surface radiation data. The monthly average of daily R n reached a minimum during the winter period followed by an increase until May and then a decline until January. This variation is consistent with solar activity. The annual mean daily total R n values were 0.92 MJ m−2 d−1 and 0.66 MJ m−2 d−1 in Lhasa and Haibei, respectively.
A relationship between R n and broadband solar radiation (R s) was demonstrated by a good linear correlation at the two sites. R n can be an accurate estimate from R s. The estimated R n values were similar to the observed values, and the relative deviations between the estimates and measurements of R n were 2.8% and 3.8% in Lhasa and Haibei, respectively. The application of the R n estimating model to other locations showed that it could provide acceptable estimated R n values from the R s data. Furthermore, we analyzed the influence of clouds on R n by different clear index (K s), defined as the ratio of R s to the extraterrestrial solar irradiance on a horizontal surface. The results indicate that more accurate results are associated with increased cloudy conditions. The influence of the albedo was also considered, but its inclusion in the model resulted in only a slight improvement. Because surface albedo is not usually measured, an expression based solely on global solar radiation could be of more extensive use.
Similar content being viewed by others
References a
lados, I., I. Foyo-Moreno, F. J. Olmo, and L. Alados-Arboledas, 2003: Relationship between net radiation and solar radiation for semi-arid shrub-land. Agricultural and Forest Meteorology, 116, 221–227.
Allen, R. G., 1996: Assessing integrity of weather data for reference evapotranspiration estimation. Journal of Irrigation and Drainage Engineering, 122, 97–106.
Allen, R. G., M. Tasumi, and R. Trezza, 2007: Satellitebased energy balance for mapping evapotranspiration with internalized calibration (METRIC). Model Journal of Irrigation and Drainage Engineering, 133, 380–394.
Blonquist, J. M. Jr., B. D. Tanner, and B. Bugbee, 2009: Evaluation of measurement accuracy and comparison of two new and three traditional net radiometers. Agricultural and Forest Meteorology, 149, 1709–1721.
Bruce, W., 1996: A new method for calibrating reference and field pyranometers. J. Atmos. Oceanic Technol., 13, 638–645.
Davies, J. A., 1966: A note on the relationship between net radiation and solar radiation. Quant. J. Roy. Meteor. Soc., 93, 109–115.
Duan, A. M., and G. X. Wu, 2005: Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia. Climate Dyn., 24, 793–807.
Elhadidy, M. A., D. Y. Abdel-Nabi, and P. D. Kruss, 1990: Ultraviolet solar radiation at Dhahran, Saudi Arabia. Solar Energy, 44, 315–319.
Fritschen, L.J., 1967: Net and solar radiation relations over irrigated field crops. Agricultural Meteorology, 4, 55–62.
Geiger, M., L. Diabate, L. Menard, and L. Wald, 2002: A web service for controlling the quality of measurements of global radiation. Solar Energy, 73 (6), 475–480.
Hu, B., Y. S. Wang, and G. R. Liu, 2007: Spatiotemporal characteristics of photosynthetically active radiation in China. J. Geophys. Res., 112, D14106, doi: 10.1029/2006JD007965.
Hu, B., Y. S. Wang, and G. R. Liu, 2008: Influences of the clearness index on UV solar radiation for two locations in the Tibetan Plateau-Lhasa and Haibei. Adv. Atmos. Sci., 25(5), 885–896, doi: 10.1007/s00376-008-0885-8.
Huber, L., and T. J. Gillespie, 1992: Modelling leaf wetness in relation to plant disease epidemiology. Annual Review of Phytopathology, 30, 553–577.
Iziomon, M. G., H. Mayer, and A. Matzarakis, 2000: Empirical models for estimating net radiation flux: a case study for three mid-latitude sites with orographic variability. Astrophysics and Space Science, 273, 313–330.
Jiang, H., and Z. Qi, 1991: The influence of surface net radiation over Lhasa region. Plateau Meteorology, 10(3), 325–331. (in Chinese)
Jegede, O. O., 1997: Daily averages of net radiation measured at Osu, Nigeria in 1995. International Journal of Climatology, 17, 1357–1367.
Kalthoff, N., M. Fiebig-Wittmaack, C. MeiBner, M. Kohler, M. Uriarte, I. Bischoff-GauB, and E. Gonzales, 2006: The energy balance, evapotranspiration and nocturnal dew deposition of an arid valley in the Andes. Journal of Arid Environments, 65, 420–443.
Kaminsky, K. Z., and R. Dubayah, 1997: Estimation of surface net radiation in the boreal forest and northern prairie from shortwave flux measurements. J. Geophys. Res., 102(D24), 29707–29716.
Kjaersgaard, J. H., R. H. Cuenca, F. L. Plauborg, and S. Hansen, 2007: Long-term comparisons of net radiation calculation schemes. Bound.-Layer Meteor., 123, 417–431.
Krishnamurti, T. N., and C. M. Kishtawal, 2000: A pronounced continental-scale diurnal mode of Asian Summer Monsoon. Mon. Wea. Rev., 128, 462–473.
Li, Y. N., W. Y. Wang, L. Zhao, X. Q. Zhao, G. M. Cao, and S. B. Shi, 2002: The characteristics of Ultraviolet radiation and its physiology effect on the plants in the area of Haibei alpine meadow of Qilian Mountain. Plateau Meteorology, 21(6), 615–621. (in Chinese)
Liu, B. Y. H., and R. C. Jordan, 1960: The interrelationship and characteristic distribution of direct, diffuse and total solar radiation. Solar Energy, 4, 1–19.
Manabe, S., and A. J. Broccoli, 1990: Mountains and arid climate of middle latitudes. Science, 247, 192–195.
Madeira, A. C., K. S. Kim, S. E. Taylor, and M. L. Gleason, 2002: A simple cloud-based energy balance model to estimate dew. Agricultural and Forest Meteorology, 111, 55–63.
Monteith, J. L., and G. Szeicz, 1961: The radiation balance of bare soil and vegetation. Quart. J. Roy. Meteor. Soc., 87, 159–170.
Neilsen, L. B., L. P. Prahm, R. Berkowicz, and K. Conradse, 1981: Net incoming radiation estimated from hourly global radiation and/or cloud observations. Journal of Climatology, 1, 255–272.
Park, M. S., C. H. Ho, J. Kim, and R. L. Elsberry, 2010: Diurnal circulations and their multi-scale interaction leading to rainfall over the South China Sea upstream of the Philippines during intraseasonal monsoon westerly wind bursts. Climate. Dyn., doi: 10.1007/s00382-010-0922-z.
Sato, T., and F. Kimura, 2007: How does the Tibetan Plateau affect the transition of Indian Monsoon rainfull? Mon. Wea. Rev., 135, 2006–2015.
Wang, K. C., and S. L. Liang, 2009: Estimation of daytime net radiation from shortwave radiation measurements and meteorological observations. J. Appl. Meter. Climatol., 48, 634–643.
Wang, Y., and Coauthors, 2008: Seasonal variations in aerosol optical properties over China. Atmospheric Chemistry and Physics Discussions, 8, 8431–8453.
Wen, D. M., 1991: Some major features of surface net radiation in the Qinghai-Xizang Plateau. Journal of Nanjing Institute of Meterology, 14(2), 151–159.
Yanai, M., C. Li, and Z. Song, 1992: Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon. J. Meteor. Soc. Japan., 70, 319–351.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Hu, B., Wang, Y. & Liu, G. Relationship between net radiation and broadband solar radiation in the Tibetan Plateau. Adv. Atmos. Sci. 29, 135–143 (2012). https://doi.org/10.1007/s00376-011-0221-6
Received:
Revised:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00376-011-0221-6