Impact of Assimilating Upper-Level Dropsonde Observations Collected during the TCI Field Campaign on the Prediction of Intensity and Structure of Hurricane Patricia (2015)

• Published in: Monthly weather review Vol. 147; no. 8; pp. 3069 - 3089
• Main Authors: Feng, Jie, Wang, Xuguang
• Format: Journal Article
• Language: English
• Published: Washington American Meteorological Society 01.08.2019
• Subjects: Aircraft; Atmospheric motion; Convection; Cyclones; Data assimilation; Data collection; Dropsonde; Dropsonde observations; Dropsondes; Heat transfer; Humidity; Hurricanes; Kinematics; Latent heat; Latent heat release; Microprocessors; Outflow; Stability; Tropical climate; Tropical cyclone intensities; Tropical cyclones; Wind; Wind observation
• ISSN: 0027-0644; 1520-0493
• DOI: 10.1175/MWR-D-18-0305.1

The dropsondes released during the Tropical Cyclone Intensity (TCI) field campaign provide high-resolution kinematic and thermodynamic measurements of tropical cyclones within the upper-level outflow and inner core. This study investigates the impact of these upper-level TCI dropsondes on analyses and prediction of Hurricane Patricia (2015) during its rapid intensification (RI) phase using an ensemble–variational data assimilation system. In the baseline experiment (BASE), both kinematic and thermodynamic observations of TCI dropsondes at all levels except the upper levels are assimilated. The upper-level wind and thermodynamic observations are assimilated in additional experiments to investigate their respective impacts. Compared to BASE, assimilating TCI upper-level wind observations improves the accuracy of outflow analyses verified against independent atmospheric motion vector (AMV) observations. It also strengthens the tangential and radial wind near the upper-level eyewall. The inertial stability within the upper-level eyewall is enhanced, and the maximum outflow is more aligned toward the inner core. Additionally, the analyses including the upper-level thermodynamic observations produce a warmer and drier core at high levels. Assimilating both upper-level kinematic and thermodynamic observations also improves the RI forecast. Compared to BASE, assimilating the upper-level wind induces more upright and inward-located eyewall convection, resulting in more latent heat release closer to the warm core. This process leads to stronger inner-core warming. Additionally, the initial warmer upper-level inner core produced by assimilating TCI thermodynamic observations also intensifies the convection and latent heat release within the eyewall, thus further contributing to the improved intensity forecasts.