Abstract
The height of the atmospheric boundary layer (ABL) plays a crucial role in the vertical transport of energy, moisture, and pollutants from the surface. We investigate the development of the convective ABL (CABL) height over a tropical coastal station and quantify its variations with the shortwave radiative flux, near-surface air temperature (Tair), soil skin temperature, soil moisture content, lower tropospheric thermal structure, and virtual potential temperature lapse rate (VPLR) during onshore and offshore flows, based on multi-year (2012–2017) observations carried out using a microwave radiometer profiler and in situ probes at Thumba (8.5° N, 77° E), located in the south-west of Indian Peninsula. The maximum CABL height increases linearly with the VPLR at the rate of 140 to 200 m per °C km−1 (correlation coefficient of 0.82 to 0.92) during different seasons. The delayed onset of daytime onshore flow results in a greater CABL height as continental conditions persist longer, allowing more CABL growth, whereas the earlier arrival of the onshore flow leads to early development of a thermal internal boundary layer with a lower CABL height. When offshore flow prevails, the CABL develops like the continental CABL, with a peak CABL height greater than that during onshore flow by about 300 m. The onset of onshore flow lowers the daytime increase in Tair by about 2 °C. Such quantifications for distinct flow conditions are very sparse over tropical coastal regions and would be useful for understanding coastal air-pollution dispersal as well as validation and improvements in numerical modelling of the CABL under different wind conditions.
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References
Anjos M, Lopes A (2019) Sea breeze front identification on the northeastern coast of Brazil and its implications for meteorological conditions in the Sergipe region. Theor Appl Climatol 137:2151–2165. https://doi.org/10.1007/s00704-018-2732-x
Anurose TJ, Subrahamanyam DB, Sunilkumar SV (2016) Two years observations on the diurnal evolution of coastal atmospheric boundary layer features over Thiruvananthapuram (8.5° N, 76.9° E). India Theor App Clim 131:77–90. https://doi.org/10.1007/s00704-016-1955-y
Arritt RW (1993) Effects of the large-scale flow on characteristic features of the sea breeze. J Appl Meteorol 32:116–125. https://doi.org/10.1175/1520-0450(1993)032%3c0116:EOTLSF%3e2.0.CO;2
Bedoya-Velásquez AE, Navas-Guzmán F, de Arruda MG, Román R, Cazorla A, Ortiz-Amezcua P, Benavent-Oltra JA, Alados-Arboledas L, Olmo-Reyes FJ, Foyo-Moreno I, Montilla-Rosero E, Hoyos CD, Guerrero-Rascado JL (2019) Seasonal analysis of the atmosphere during five years by using microwave radiometry over mid-latitude site. Atmos Res 218:78–89. https://doi.org/10.1016/j.atmosres.2018.11.014
Chen W, Kuze H, Uchiyama A, Suzuki Y, Takeuchi N (2001) One-year observation of urban mixed layer characteristics at Tsukuba, Japan using a micro pulse lidar. Atmos Environ 35:4273–4280. https://doi.org/10.1016/S1352-2310(01)00181-9
Cimini D, Campos E, Ware R, Albers S, Graziano G, Oreamuno J, Joe P, Koch S, Cober S, Westwater ER (2011) Thermodynamic atmospheric profiling during the 2010 winter Olympics using ground-based microwave radiometry. IEEE Trans Geosci Remote Sens 49:4959–4969. https://doi.org/10.1109/TGRS.2011.2154337
Coen MC, Praz C, Haefele A, Ruffieux D, Kaufmann P, Calpini B (2014) Determination and climatology of the planetary boundary layer height above the Swiss plateau by in situ and remote sensing measurements as well as by the COSMO-2 model. Atmos Chem Phy 14:13205–13221. https://doi.org/10.5194/acp-14-13205-2014
Dang R, Li H, Liu Z, Yang Y (2016) Statistical analysis of relationship between daytime lidar-derived planetary boundary layer height and relevant atmospheric variables in the semiarid region in northwest China. Adv Meteorol. https://doi.org/10.1155/2016/5375918
Davis EV, Rajeev K, Mishra MK (2020) Effect of clouds on the diurnal evolution of the atmospheric boundary-layer height over a tropical coastal station. Boundary-Layer Meteorol 175:135–152. https://doi.org/10.1007/s10546-019-00497-6
Davy R (2018) The climatology of the atmospheric boundary layer in contemporary global climate models. J Clim 31:9151–9173. https://doi.org/10.1175/JCLI-D-17-0498.1
De Tomasi F, Miglietta MM, National I, Perrone MR (2011) The growth of the planetary boundary layer at a coastal site: a case study. Boundary-Layer Meteorol 139:521–541. https://doi.org/10.1007/s10546-011-9592-6
Delbarre H, Augustin P, Saïd F, Campistron B, Bénech B, Lohou F, Puygrenier V, Moppert C, Cousin F, Fréville P, Fréjafon E (2005) Ground-based remote sensing observation of the complex behaviour of the Marseille boundary layer during ESCOMPTE. Atmos Res 74:403–433. https://doi.org/10.1016/j.atmosres.2004.04.007
Driedonks AGM (1982) Models and observations of the growth of the atmopsheric bundary layer. Boundary-Layer Meteorol 23:283–306. https://doi.org/10.1007/BF00121117
Fan K, Zhang Q, Singh VP, Sun P, Song C, Zhu X, Yu H, Shen Z (2019) Spatiotemporal impact of soil moisture on air temperature across the Tibet Plateau. Sci Total Environ 649:1338–1348. https://doi.org/10.1016/j.scitotenv.2018.08.399
Garratt JR (1992) The atmospheric boundary layer. Cambridge University Press, Cambridge USA
Gelaro R, McCarty W, Suárez MJ, Todling R, Molod A, Takacs, L, Randles CA, Darmenov A, Bosilovich MG, Reichle R, Wargan K, Coy L, Cullather R, Draper C, Akella S, Buchard V, Conaty A, da Silva AM, Gu W, Kim G, Koster R, Lucchesi R, Merkova D, Nielsen JE, Partyka G, Pawson S, Putman W, Rienecker M, Schubert SD, Sienkiewicz M, Zhao B (2017) The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2). J Clim 30(14):5419–5454. https://doi.org/10.1175/JCLI-D-16-0758.1
Güldner J, Spankuch D (2001) Remote sensing of the thermodynamic state of the atmospheric boundary layer by microwave radiometry. J Atmos Oceanic Technol 18:925–933. https://doi.org/10.1175/1520-0426(2001)018%3c0925:RSOTTS%3e2.0.CO;2
Han Y, Westwater ER (2000) Analysis and improvement of tipping calibration for ground based microwave radiometers. IEEE Trans Geosci Remote Sens 38:1260–1276. https://doi.org/10.1109/36.843018
Knupp K, Ware R, Cimini D, Vandenberghe F, Vivekanandan J, Westwater ER, Coleman T (2009) Ground-based passive microwave profiling during dynamic weather conditions. J Atmos Ocean Technol 26:1057–1073
Kunhikrishnan PK, Sen Gupta K, Ramachandran R, Prakash JWJ, Nair KN (1993) Structure of the thermal internal boundary layer over Thumba, India. Ann Geophys 11:52–60
Kuwagata T, Kondo J, Sumioka M (1994) Thermal effect of the sea breeze on the structure of the boundary layer and the heat budget over land. Boundary-Layer Meteorol 67:119–144. https://doi.org/10.1007/BF00705510
Liu J, Pu Z (2019) Does soil moisture have an influence on near-surface temperature? J Geophy Res Atmos 124:6444–6466. https://doi.org/10.1029/2018JD029750
Lokoshchenko MA (2002) Long-term sodar observations in Moscow and a new approach to potential mixing determination by radiosonde data. J Atmos Ocean Technol 19:1151–1162. https://doi.org/10.1175/1520-0426(2002)019%3c1151:LTSOIM%3e2.0.CO;2
Mauder M, Foken T, Cuxart J (2020) Surface energy balance closure over land: a review. Boundary-Layer Meteorol 177:395–426. https://doi.org/10.1007/s10546-020-00529-6
Miller STK, Keim BD, Talbot RW, Mao H (2003) Sea breeze: structure, forecasting, and impacts. Rev Geophys 41(3):1011. https://doi.org/10.1029/2003RG000124
Molod A, Salmun H, Dempsey M (2015) Estimating planetary boundary layer heights from NOAA profiler network wind profiler data. J Atmos Ocean Technol 32:1545–1561. https://doi.org/10.1175/JTECH-D-14-00155.1
Moreira GdA, Guerrero-Rascado JL, Bravo-Aranda JA, Foyo-Moreno I, Cazorla A, Alados I, Lyamani H, Landulfo E, Alados-Arboledas L (2020) Study of the planetary boundary layer height in an urban environment using a combination of microwave radiometer and ceilometer. Atmos Res 240:104932. https://doi.org/10.1016/j.atmosres.2020.104932
Pal S, Haeffelin M (2015) Forcing mechanisms governing diurnal, seasonal, and interannual variability in the boundary layer depths: five years of continuous lidar observations over a suburban site near Paris. J Geophys Res Atmos 120:11936–11956. https://doi.org/10.1002/2015JD023268
Pal S, Lee TR (2019) Contrasting air mass advection explains significant differences in boundary layer depth seasonal cycles under onshore versus offshore flows. Geophys Res Lett 46:2846–2853. https://doi.org/10.1029/2018GL081699
Papanastasiou DK, Melas D, Bartzanas T, Kittas C (2010) Temperature, comfort and pollution levels during heat waves and the role of sea breeze. Int J Biometeorol 54:307–317. https://doi.org/10.1007/s00484-009-0281-9
Rajeev K, Mishra MK, Sunilkumar SV, Sijikumar S (2016) Dual polarization micropulse lidar observations of the diurnal evolution of atmospheric boundary layer over a tropical coastal station. In: Proc. SPIE, Lidar remote sensing for environmental monitoring XV 98790. https://doi.org/10.1117/12.2228049
Raju CS, Renju R, Antony T, Mathew N, Moorthy KK (2013) Microwave radiometric observation of a waterspout over coastal Arabian Sea. IEEE Geosci Remote Sens Lett 10:1075–1079. https://doi.org/10.1109/LGRS.2012.2229960
Ramachandran R, Prakash JWJ, Gupta KS, Nair KN, Kunhikrishnan PK (1994) Variability of surface roughness and turbulence intensities at a coastal site in India. Boundary-Layer Meteorol 70:385–400. https://doi.org/10.1007/BF00713777
Reddy BR, Srinivas CV, Shekhar SSR, Baskaran R, Venkatraman B (2020) Impact of land surface physics in WRF on the simulation of sea breeze circulation over southeast coast of India. Meteorol Atmos Phys 132:925–943. https://doi.org/10.1007/s00703-020-00726-5
Renju R, Raju CS, Mathew N, Antony T, KrishnaMoorthy K (2015) Microwave radiometer observations of interannual water vapor variability and vertical structure over a tropical station. J Geophys Res Atmos 120:4585–4599. https://doi.org/10.1002/2014JD022838
Renju R, Raju CS, Mishra MK, Mathew N, Rajeev K, Moorthy KK (2017) Atmospheric boundary layer characterization using multiyear ground-based microwave radiometric observations over a tropical coastal station. IEEE Trans Geosci Remote Sens 55:6877–6882. https://doi.org/10.1109/TGRS.2017.2735626
Schmid P, Niyogi D (2012) A method for estimating planetary boundary layer heights and its application over the ARM southern great plains site. J Atmo Ocean Technol 29:316–322. https://doi.org/10.1175/JTECH-D-11-00118.1
Seibert P, Beyrich F, Gryning SE, Joffre S, Rasmussen A, Tercier P (2000) Review and intercomparison of operational methods for the determination of the mixing height. Atmos Environ 34:1001–1027. https://doi.org/10.1016/S1352-2310(99)00349-0
Seidel DJ, Ao CO, Li K (2010) Estimating climatological planetary boundary layer heights from radiosonde observations: comparison of methods and uncertainty analysis. J Geophys Res Atmos 115:1–15. https://doi.org/10.1029/2009JD013680
Simpson JE, Mansfield DA, Milford JR (1977) Inland penetration of sea-breeze fronts. Q J R Meteorol Soc 103:47–76. https://doi.org/10.1002/qj.49710343504
Stull RB (1988) An introduction to boundary layer meteorology. Kluwer Academic Publishers, Dordrecht/Boston/London
Svensson G, Holtslag AAM, Kumar V, Mauritsen T, Steeneveld GJ, Angevine WM, Bazile E, Beljaars A, de Bruijn EIF, Cheng A, Conangla L, Cuxart J, Ek M, Freedman F, Kitagawa H, Larson VE, Lock A, Mailhot J, Masson V, Park S, Pleim J, Söderberg S, Weng W, Zampieri M (2011) Evaluation of the diurnal cycle in the atmospheric boundary layer over land as represented by a variety of single-column models: the second GABLS experiment. Boundary-Layer Meteorol 140:177–206. https://doi.org/10.1007/s10546-011-9611-7
Tucker SC, Senff CJ, Weickmann AM, Brewer WA, Banta RM, Sandberg SP, Law DC, Hardesty RM (2009) Doppler lidar estimation of mixing height using turbulence, shear, and aerosol profiles. J Atmos Ocean Technol 26:673–688. https://doi.org/10.1175/2008JTECHA1157.1
Von EA, Teixeira J (2013) A planetary boundary layer height climatology derived from ECMWF reanalysis data. J Clim 26:6575–6590. https://doi.org/10.1175/JCLI-D-12-00385.1
Wang X, Wang K (2016) Homogenized variability of radiosonde-derived atmospheric boundary layer height over the global land surface from 1973 to 2014. J Clim 29:6893–6908. https://doi.org/10.1175/JCLI-D-15-0766.1
Wang Y, Di Sabatino S, Martilli A, Li Y, Wong MS, Gutiérrez E, Chan PW (2017) Impact of land surface heterogeneity on urban heat island circulation and sea-land breeze circulation in Hong Kong. J Geophys Res Atmos 122:4332–4352. https://doi.org/10.1002/2017JD026702
Ware R, Solheim F, Carpenter R, Gueldner J, Liljegren J, Vandenberghe FA (2003) Multi-channel radiometric profiler of temperature, humidity and cloud liquid. Radio Sci 38(4):8079. https://doi.org/10.1029/2002RS002856
Ware R, Cimini D, Campos E, Giuliani G, Albers S, Nelson M, Koch SE, Joe P, Cober S (2013) Thermodynamic and liquid profiling during the 2010 winter Olympics. Atmos Res 132–133:278–290. https://doi.org/10.1016/j.atmosres.2013.05.019
Wu P, Mori S, Syamsudin F (2018) Land-sea surface air temperature contrast on the western coast of Sumatra Island during an active phase of the Madden–Julian oscillation. Prog Earth Planet Sci 5:4. https://doi.org/10.1186/s40645-017-0160-7
Wulfmeyer V, Hardesty RM, Turner DD, Behrendt A, Cadeddu MP, Di Girolamo P, Schlüssel P, Van Baelen J, Zus F (2015) A review of the remote sensing of lower tropospheric thermodynamic profiles and its indispensable role for the understanding and the simulation of water and energy cycles. Rev Geophys 53:819–895. https://doi.org/10.1002/2014RG000476
Zhang N, Chen Y, Zhao W (2012) Lidar and microwave radiometer observations of planetary boundary layer structure under light wind weather. J Appl Remote Sens 6:63513–63518. https://doi.org/10.1117/1.JRS.6.063513
Zhang HS, Zhang XY, Li QH, Cai X, Fan S, Song Y, Hu F, Che H, Quan J, Kang L, Zhu T (2020) Research progress on estimation of the atmospheric boundary layer height. J Meteorol Res 34(3):482–498. https://doi.org/10.1007/s13351-020-9910-3
Acknowledgements
The authors thank C. Suresh Raju, SPL, for providing the microwave radiometer profiler data during 2012–2017. MERRA-2 data are available at the Modeling and Assimilation Data and Information Services Center (MDISC), managed by the NASA Goddard Earth Sciences (GES) Data and Information Services Center (DISC). Digital elevation map is accessed through https://topotools.cr.usgs.gov/GMTED_viewer/gmted2010_fgdc_metadata.html. We thank the anonymous reviewers for their very constructive comments and suggestions, which improved the content of this paper.
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Davis, E.V., Rajeev, K. & Sambhu Namboodiri, K.V. The Convective-Atmospheric-Boundary-Layer Height and its dependence upon Meteorological Variables At a Tropical Coastal Station during Onshore and Offshore Flows. Boundary-Layer Meteorol 183, 143–166 (2022). https://doi.org/10.1007/s10546-021-00665-7
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DOI: https://doi.org/10.1007/s10546-021-00665-7