Sarah Kaplan

Washington, D.C. Sarah Kaplan is a climate and science reporter for The Washington Post. She covers humanity's response to a warming world and the impacts of climate change on Earth's systems and ecosystems. She joined The Post in 2019 after working as an environment writer at CNN, where she covered topics such as hurricanes, wildfires, droughts, floods, volcanoes and asteroids. She has also written about space weather and the sun's influence on Earth. Kaplan holds a bachelor of science in international culture and politics from Georgetown University. She is based in Washington, D.C., but travels frequently to report on climate stories around the world.

83%

The Daily's Verdict

This author has a mixed reputation for journalistic standards. It is advisable to fact-check, scrutinize for bias, and check for conflicts of interest before relying on the author's reporting.

Bias

100%

Examples:

  • The article does not show any signs of bias in favor of or against any side on the issue of climate change.

Conflicts of Interest

100%

Examples:

Contradictions

50%

Examples:

  • There are no major contradictions found in the article regarding the author's sources, claims, or arguments.

Deceptions

50%

Examples:

  • The article does not appear to be deceptive in its presentation of information or use of rhetorical techniques.

Recent Articles

The Complex System of the Atlantic Meridional Overturning Circulation: How it Transports Water, Heat and Nutrients Throughout the Ocean

The Complex System of the Atlantic Meridional Overturning Circulation: How it Transports Water, Heat and Nutrients Throughout the Ocean

Broke On: Saturday, 10 February 2024 The Atlantic Meridional Overturning Circulation (AMOC) is a complex system that transports water, heat and nutrients throughout the Atlantic Ocean. It starts near the equator where surface of ocean is warmed by tropical sun and as it moves northward some of it evaporates which increases salt concentration (density) of remaining water. By time water nears Greenland it has cooled down making its density even more dense, this cold salty water sinks to seafloor pushing the other parts out of path. Displaced part flows south along ocean bottom and once returns to tropics is drawn back to surface through upwelling process which starts cycle again.