The Nature of Transition Circumstellar Disks III. Perseus, Taurus, and Auriga

TL;DR

This study characterizes 74 transition disks across Perseus, Taurus, and Auriga, classifying their types and analyzing their properties to understand disk evolution and planet formation mechanisms.

Contribution

It provides a homogeneous classification of transition disks using multi-wavelength data, linking disk properties to their evolutionary stages and planet formation processes.

Findings

Disk age distribution supports core accretion for giant planet formation.

Identified different disk categories with specific physical characteristics.

Estimated formation timescale for giant planets is 2-3 million years.

Abstract

As part of an ongoing program aiming to characterize a large number of Spitzer-selected transition disks (disks with reduced levels of near-IR and/or mid- IR excess emission), we have obtained (sub)millimeter wavelength photometry, high-resolution optical spectroscopy, and adaptive optics near-infrared imaging for a sample of 31 transition objects located in the Perseus, Taurus, and Auriga molecular clouds. We use these ground-based data to estimate disk masses, multiplicity, and accretion rates in order to investigate the mechanisms potentially responsible for their inner holes. Following our previous studies in other regions, we combine disk masses, accretion rates and multiplicity data with other information, such as SED morphology and fractional disk luminosity to classify the disks as strong candidates for the following categories: grain-growth dominated disks (7 objects), giant planet-forming disks (6 objects), photoevaporating disks (7 objects), debris disks (11 objects), and cicumbinary disks (1 object, which was also classified as a photoeavaporating disk). Combining our sample of 31 transition disks with those from our previous studies results in a sample of 74 transition objects that have been selected, characterized, and classified in an homogenous way. We discuss this combined high-quality sample in the context of the current paradigm of the evolution and dissipation of protoplanetary disks and use its properties to constrain different aspects of the key processes driving their evolution. We find that the age distribution of disks that are likely to harbor recently formed giant planets favors core accretion as the main planet formation mechanism and a ~2-3 Myr formation timescale