One of the big unknowns of the pulse flow of water currently working its way down the channel of the Colorado River in its delta is whether that water will reach the sea. The mouth of the Colorado River drained historically into the Upper Gulf of California (Sea of Cortez), a unique body of water that Jacques Cousteau called “the world’s aquarium.” But with dams and diversions of Colorado River water serving a population of more than 35 million in the United States and Mexico, the Colorado River hasn’t reached its destination regularly since before 1960.
The pulse flow started on March 23, and will continue through May 18. The flow rate varies over time, by design meant to inundate the channel and later to recede slowly and stimulate germination of the seeds that will grow into native cottonwood and willow trees. In order to do this work the pulse flow waters must travel some 25 miles (40 kilometers) of sand that typically exist in the midst of the river’s 100-mile (160-kilometer) run in its delta.
We have been watching this progress for days, cheering its advance. Run river run!
Progress has been slow but steady.
On the first day of the release we found cool, clear water advancing down the channel some 17 river miles (27 kilometers) below Morelos Dam. The “front” moved quickly where the channel is typically wetted – even filled with standing water – due to a high groundwater table. Since then, it has been crossing the sand, and significant volumes of water soak into the ground, recharging a depleted groundwater aquifer.
The map shows its progress, slow because of its need to saturate the sand as it goes, because of the low gradient in the flat delta, and because of the considerable presence of scrub brush (mostly non-native salt cedar) growing in the channel.
The pulse flow’s behavior has been hard to predict. The river hasn’t flowed here in years, and moreover, no federal agency in the United States or Mexico had viewed the delta as its responsibility, so no agency had studied the delta in recent decades.
But now the United States and Mexico, in addition to implementing the pulse flow, are funding an extensive monitoring program, gathering information on how the water moves, how the channel changes, how the trees grow, and what the wildlife does as a result of the pulse flow. Dozens of U.S. and Mexican scientists are spending their days collecting data that will be crucial to fleshing out our understanding of the pulse flow. They are a hardy crew!
I’m grateful for their efforts as they brave hot sun and dense scrub to take samples and measurements that will tell the pulse flow story and help us improve how we design any future pulse flows (we will also need a new U.S.-Mexico agreement for that).
I have been visiting the front of the pulse flow nearly every day, and yesterday I had the extreme good fortune to see the front finish its journey down the sand. The leading edge of the water finally arrived at the middle reach of the delta where groundwater is typically found in the channel.
Looking upstream, we watched the pulse flow creep forward. Looking downstream, we watched the groundwater creep up the channel. And eventually they met, marking the end of the pulse flow’s slow advance over the sand.
Now that the dry reach has been saturated, we expect water to move more speedily. The leading edge of the pulse flow will now travel the middle and lower reaches of the delta, reaches that are typically wet due to high groundwater and drainage from nearby agricultural fields. Infiltration will not be nearly as great, and the water should run rather than creep. The pulse flow still has miles to go, but these miles should be easier to travel.
Will the pulse flow reconnect the Colorado River to the sea? We still don’t know. We don’t even know that we’ll be able to see it when it does. But scientists will be out there taking conductivity measurements, and will tell us if, and when, water at the river’s mouth becomes less salty as freshwater arrives.
Flow river flow!