The CTD Cast: How Oceanographers Read a Column of Water
A CTD cast reads temperature, salt and depth through the whole water column. Inside the instrument that gave oceanography its vertical vision.
Dr. Lena Fischer ·
9 articles
A CTD cast reads temperature, salt and depth through the whole water column. Inside the instrument that gave oceanography its vertical vision.
Dr. Lena Fischer ·
Estuaries layer fresh water over salt in shifting gradients. How estuarine circulation works, where kelp's brackish limit lies, and why the river–sea edge matters.
Dr. Theo Nakamura ·
River plumes deliver nutrients that feed kelp forests — and floods that smother them in sediment and fresh water. The double-edged physics of the river mouth.
Dr. Lena Fischer ·
Why the sea is salty, why it's slightly alkaline, and why its pH is drifting. A gentle but rigorous introduction to the chemistry that rules marine life.
Dr. Lena Fischer ·
An atmospheric river can drop farm salinity for weeks. How seaweed farmers monitor freshwater events, protect stock and learn each site's local limits.
Naomi Reyes ·
Thermoclines, haloclines and pycnoclines are the invisible boundaries that slice the sea into layers. What they are, how they form, and why they run coastal life.
Dr. Lena Fischer ·
How seaweed farmers should read temperature, salinity and nitrate: practical sensor routines, thermocline effects and simple decision rules for kelp growth.
Naomi Reyes ·
A coastal atlas guide to the Baltic Sea, where salinity drops below what most kelp can survive and bladderwrack forests rule a brackish inland sea.
Dr. Mara Ellison ·
Why is the sea salty, why is some sea fresher than the rest, and why does salt settle into layers? The ocean's salt budget and haloclines, explained.
Dr. Lena Fischer ·