Correction to: Daytime Convective Boundary-Layer Evolution on Three Fair-Weather Days in CASES-97.

Comparison of the profiler HT <math xmlns="http://www.w3.org/1998/Math/MathML"><mrow><mi>W</mi><mfenced close=")" open="("><msub><mi>h</mi><mn>1</mn></msub></mfenced></mrow></math> ht to that from radiosonde data in Fig. Figure 1 shows the synoptic-forcing terms in the equation for HT <math xmlns="http://www.w3.org/1998/Math/MathML"><msub><mi>h</mi><mn>1</mn></msub></math> ht time tendency, 1 HT <math display="block" xmlns="http://www.w3.org/1998/Math/MathML"><mrow><mfrac><mrow><mi mathvariant="normal"> </mi><msub><mi>h</mi><mn>1</mn></msub></mrow><mrow><mi mathvariant="normal"> </mi><mi>t</mi></mrow></mfrac><mo>=</mo><msub><mi>w</mi><mi>e</mi></msub><mo>+</mo><mi>W</mi><mfenced close=")" open="("><msub><mi>h</mi><mn>1</mn></msub></mfenced><mo>-</mo><mi>U</mi><mfenced close=")" open="("><msub><mi>h</mi><mn>1</mn></msub></mfenced><mfrac><mrow><mi mathvariant="normal"> </mi><msub><mi>h</mi><mn>1</mn></msub></mrow><mrow><mi mathvariant="normal"> </mi><mi>x</mi></mrow></mfrac><mo>-</mo><mi>V</mi><mfenced close=")" open="("><msub><mi>h</mi><mn>1</mn></msub></mfenced><mfrac><mrow><mi mathvariant="normal"> </mi><msub><mi>h</mi><mn>1</mn></msub></mrow><mrow><mi mathvariant="normal"> </mi><mi>y</mi></mrow></mfrac><mo>,</mo></mrow></math> ht Graph where HT <math xmlns="http://www.w3.org/1998/Math/MathML"><msub><mi>w</mi><mi>e</mi></msub></math> ht represents CBL growth due to entrainment and the last two terms represent horizontal advection, assuming HT <math xmlns="http://www.w3.org/1998/Math/MathML"><msub><mi>h</mi><mn>1</mn></msub></math> ht is parallel to the plane described by the three sounding sites. 11 of LeMone et al. ([2]) confirms strong subsidence starting around 1700 UTC (1100 LST), with HT <math xmlns="http://www.w3.org/1998/Math/MathML"><mrow><mi>W</mi><mfenced close=")" open="("><msub><mi>h</mi><mn>1</mn></msub></mfenced></mrow></math> ht decreasing with time between 1630 and 1900 UTC. [Extracted from the article]