First forest canopy heights from NASA’s ICESat mission

Posted on June 29, 2019June 29, 2019 by Geoff Zeiss

First terrain surface and canopy heights from ICESat-2

Launched in September 2018, ICESat-2 (Ice, Cloud, and land Elevation Satellite-2) has just begun making its first data available. The data map global terrain surface and forest canopies. The Advanced Topographic Laser Altimeter System (ATLAS) instrument on-board ICESat-2 utilizes photon counting technology for the altimetry observations. Photon counting technology is relatively new to the vegetation mapping community. Data from ICESat-2 will provide global terrain elevation and canopy height estimates as well as showing potential for estimation of forest biomass.

The ATL08 land and vegetation product for the ICESat-2 Mission, Amy Neuenschwander, Katherine Pitts Remote Sensing of Environment, 221, February 2019, Pages 247-259 doi/10.1016/j.rse.2018.11.005

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From Our Files

Synchronization of North Pacific and North Atlantic climates and abrupt warming during last deglaciation

For most of the past 18,000 years warm temperatures in the North Pacific often correspond to cold temperatures in the North Atlantic and vice versa. In this study it is revealed that the occasional synchronicity in the North Pacific and North Atlantic climates correspond to periods of abrupt Northern Hemisphere warming.

Evidence of CO2 outgassing from the Southern Ocean early in the last deglaciation

During the last deglaciation atmosphere CO2 concentration rose by about 80 ppm amplifying climate warming. This study of radiocarbon in deep sea corals found that Southern ocean deep water was radiocarbon-depleted throughout the last ice age, but this depletion disappeared between 16,600 and 14,600 years ago consistent with Southern Ocean CO2 outgassing that corresponded to the first pulse of increased atmospheric CO2 early in the deglaciation.

Global deep ocean temperature 60 million years ago to present

New evidence that CO2 may have driven cooling 50-30 million years ago

New evidence from analyzing fossil plankton shells has revealed that CO2 concentration in the Earth’s atmosphere was about triple current levels around 52 million years ago. It then declined to levels close to current atmospheric CO2 concentration 34 million years ago when Antarctica began to glaciate.

Simple rule accounts for onset of ice age deglaciations over the past three million years

A recent study has created a simple mathematical rule that can account for the timing of the onset of interglacials following ice ages over the past three million years. The rule is based on predictable long-term astronomical variations in the Earth’s orbit and tilt called Milankovitch cycles.

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