Dhangar, NG; Lal, DM; Ghude, SD; Kulkarni, R; Parde, AN; Pithani, P; Niranjan, K; Prasad, DSVVD; Jena, C; Sajjan, VS; Prabhakaran, T; Karipot, AK; Jenamani, RK; Singh, S; Rajeevan, M (2021). On the Conditions for Onset and Development of Fog Over New Delhi: An Observational Study from the WiFEX. PURE AND APPLIED GEOPHYSICS, 178(9), 3727-3746.
Abstract
Dense fog events and their micrometeorological characteristics and structural evolution at Indira Gandhi International Airport (IGIA), New Delhi, during the Winter Fog Experiment (WiFEX) are illustrated in this study. Four dense fog events that occurred in January 2016 for which visibility dropped below 200 m have been selected. Depending on the visibility and micrometeorological structure, the fog processes were classified into (i) an initial formation as a thermally stable optically thin fog and (ii) a subsequent mature, weakly unstable deep fog. Surface radiative cooling supported by a deep saturated layer in the nocturnal surface layer promotes the rapid development and intensification of the initial shallow fog into the extremely dense fog. Optically thin fog appeared to develop when a thin saturated layer of air formed near the ground under low-turbulence kinetic energy (< 0.1 m(2)/s(2)). The fog was sustained in the optically thin phase until the air at 20 m remained in a sub-saturated condition in the thermally stable surface layer. Furthermore, when the saturated layer near the surface progressively expanded upward as a result of sustained cooling inside the shallow fog, it rapidly transformed into an extremely dense fog. The threshold for transition from the optically thin phase to extremely dense phase appeared when the air at 20 m neared the saturation point. The dense fog observations for all cases indicate that when the saturated layer was deeper than 20 m, the fog was able to withstand larger turbulence intensity (TKE values between 0.4 m(2)/s(2) and 0.5 m(2)/s(2)).
DOI:
10.1007/s00024-021-02800-4
ISSN:
0033-4553