This section will analyze and discuss the error distribution of the TC intensity estimation model and the fitting performance of MSW and MSLP in various basins. The first part explores the error distribution within a single basin across various intensity categories. In the second part, we explore ...
Section 4 discusses the role of external forcing, while Sect. 5 focuses on the internal variability. Section 6 shows the sensitivity experiments designed to help understanding the mechanisms. Finally, Sect. 7 devotes conclusions and discussions. 2 Data, model simulations and methods 2.1 Data In ...
Tropical Storm Sara began as a low-pressure system in the western Caribbean around November 11, 2024. From its formation, the National Hurricane Center warned of its potential development due to favorable conditions in the region, such as high humidity and warm sea surface temperatures. On Novembe...
In Section 2 we summarize recent work that demonstrates close relationships between ITCZ position, AHTEQ and tropical SST gradients in the modern seasonal cycle and in models of altered climate states (Donohoe et al., 2013), providing a means for using past SST gradients to reconstruct changes ...
Section 3 describes in detail the formulas to derive Root Mean Squared Error (RMSE) and Correlation Coefficient (CC) from the TC method; Section 4 analyzes the results from a broad overview and further examines the specific event (Hurricane Harvey); and Section 5 provides the conclusions and fu...
of global ocean vector winds on six-hour intervals that are closely tied to satellite measurements. The current versions of CCMP are fairly accurate at low to moderate wind speeds (<15 m/s) but are systematically too low at high winds at locations/times where a collocated satellite measurement...
This section provides an explanation of various methods. DeepNAO: The DeepNAO model is a software architecture that integrates the generalised additive model (GAM) with deep learning techniques. GAMs are a variant of linear regression that replacing the linear components with smooth transformations of...
Figure 3. (a) The RHI spectral width scan and (b) the associated cross-section of the eddy dissipation rate (EDR) as well as (c) the three-dimensional wind fields (left: horizontal wind field at height of around 34 m above sea level. Right: wind field projected on the cross-sectiona...
Indeed, the impact of the 2016 bleaching event was the greatest on the northern section of the GBR [2], which might not have been picked up in our analysis grouping reefs of various latitudes into three cross-shelf positions. Another possible explanation is that the impact of the 2016 ...
Conclusions are summarized in Section 6. 2. Dataset In this study, 19 Sentinel-1A VH-polarized EW mode images under tropical cyclone conditions are collected. The matching SMAP radiometer wind speeds are collected for comparison and model validation. The data are divided into two datasets. Dataset...