100 Years of Progress in Tropical Cyclone Research in: Meteorological Monographs
Volume 59 Issue 1 (2018) Jump to Content Logo Logo Logo Logo Logo Logo JOURNALS …

Dominant climatic factors controlling the lifetime peak intensity of typhoons are determined
from six decades of Pacific typhoon data. We find that upper ocean temperatures in the low …

Turbulence-enhanced mixing of upper ocean heat allows interaction between the tropical
atmosphere and cold water masses that impact climate at higher latitudes thereby regulating …

Tropical cyclones (TCs) are hazardous natural disasters. Because TC intensification is
significantly controlled by atmosphere and ocean environments, changes in these …

The ocean temperature response to tropical cyclones (TCs) is important for TC development,
local air–sea interactions, and the global air–sea heat budget and transport. The modulation …

Compound hazards are more destructive than the individual ones. Using observational and
reanalysis datasets during 1960–2019, this study shows a remarkable concurrent …

Tropical cyclones generate a large and wide cold wake along their trajectories, which
conditions the subsequent evolution of the tropical cyclone themselves. The cold wakes …

In situ observation of a buoys/moorings array and a model simulation were used to study the
modulation of upper ocean thermal structure by Typhoon Kalmaegi in September 2014. The …

Tropical cyclones can pump heat into the ocean by producing a long‐lasting subsurface
warm anomaly while leaving a relatively short‐term surface cold anomaly via mixing the …

The effect of tropical cyclone (TC) size on TC-induced sea surface temperature (SST)
cooling and subsequent TC intensification is an intriguing issue without much exploration …