California current warm or cold

A shaded courtyard at Esperanza Elementary School in Los Angeles provides a way for students to spend time outside while escaping the heat. V. Kelly Turner UCLA Luskin Center for Innovation As hot days become A “Obviously, the California Education Board wasn’t set up to think about climate change. But now that climate change is a reality, virtually every sector is going to have to think about it,” said V. Kelly Turner, an urban planning associate professor and the director of the Luskin Center. The center’s recommendations include steps such as setting an indoor temperature limit, documenting the air-conditioning and shade infrastructure of each school, and investing in shade and greenery for play areas. The brief also calls out areas needing more research, such as the safest indoor temperature range. The best way to keep kids cool is perhaps the most obvious: providing shade, which can reduce the heat stress experienced throughout the day by 25% to 35%, according to That requires reconfiguring playgrounds to make them cooler, said Perry Sheffield, a pediatrician and an environmental medicine researcher at Mount Sinai in New York City. In addition to shade, swapping heat-absorbing materials like asphalt and rubber for grass and wood chips helps cool things down. “The more we can encourage play as well as physical activity, the healthier our kids are going to be, so figuring out a way to do that safely is really key,” said Sheffield. On a playground in the San Fernando Vall...

The temperature and salinity of its waters vary with seasonal variations in upwelling, insolation, and flow. The maximum ranges in temperature and salinity from its northern to its southern end are 48° to 79° F (9° to 26° C) and 32.5 to 34.5 parts per thousand, respectively. During the summer, when upwelling is most dominant, a countercurrent below 650 ft develops close to the coast. The cold upwelling water brings rich nutrients to the surface and

An area of high pressure over the central Pacific Ocean will begin to tilt toward the West Coast on Tuesday, reeling in the start of a warming trend over parts of the Bay Area. Baron/Lynx An oddly-shaped area of high pressure is forecast to sprinkle parts of the Bay Area with pockets of warm air as it noses toward the Pacific Northwest on Tuesday. Inland commuters might notice some of the changes in the weather in the afternoon, but one region will warm faster than the rest. A “nosy” weather system Highs and lows usually take on shapes that look like the circles on graphics, but that won’t be the case on Tuesday. The European weather model signals an area of higher atmospheric pressure at around 5,000 feet above the ground, which is in line with the tilt of the high pressure system forecast for the week. Weatherbell The uneven warming trend forecast for Tuesday in the Bay Area has to do with the oval, nose-like shape of the high-pressure system. Like someone squishing Play-Doh, shifts in the flow of air in the atmosphere can alter the shapes and sizes of weather systems. The high-pressure system will poke into the North Bay’s inland valleys, bringing warm, dry air that will quickly raise the temperature in cities like Napa and Petaluma by as much as 5 to 7 degrees compared with Monday. The East Bay and South Bay will also experience some warming — 2 to 3 degrees — but not as much as their northern counterparts. The high-pressure system’s uneven shape on Tuesday means it wo...

Table of Contents • • • • • • • • • • • • • • • • • • • • • • • • • • • • • Which way does the California Current flow? The California Current is a cold water Pacific Ocean current that moves southward along the western coast of North America, beginning off southern British Columbia and ending off southern Baja California Sur. How deep is California Current? 500 m The California Current proper is a year-round equatorward flow extending seaward from the shelfbreak to a distance of ~1000 km, with strongest speeds at the surface and extending to at least 500 m depth. 320 It carries cooler, fresher, nutrient-rich water equatorward. What is the California countercurrent? The Southern California Counter-current brings warm water from Baja California up along the mainland coast, swirling around Santa Barbara, Anacapa, and eastern Santa Cruz Islands. This warmer water supports biological communities reminiscent of southern California down to northern Mexico. Read More: Is bitumen a natural resource? Does the California Current flow clockwise? Garbage that reaches the ocean from the west coast of the United States and from the east coast of Japan is carried by currents—including the California Current, the North Equatorial Current, the North Pacific Current, and the Kuroshio—into the North Pacific subtropical gyre, the clockwise rotation of which draws in … Is the California Current fast or slow? Schwartzlose: The average speed of the general California Current is about 4 to 4 knot...

Updated at 10:50 a.m. ET on June 13, 2023 In the past six years, California has logged three of its five deadliest fires on record, and eight of its 10 biggest. More than 100 people have died, tens of thousands have been displaced, and millions more have been subjected to smoky air, the We know that climate change supercharges these fires thanks to the drier environments it creates, but by how much is tricky to say. Fire science is a complicated thing: A blaze might arise from a lightning strike, a hot car on tall summer grass, snapped power lines. But a Proceedings of the National Academy of Sciences delivers a fuller sense of the relationship between human-caused warming and California’s wildfires. It finds that climate change is responsible for almost all of the increase in scorched acreage during the state’s summer fires over the past 50 years. And its authors predict that the increase in burned area will only continue in the decades to come. The arrival of this study is a timely reminder just days after East Coasters endured a Using data from 1971 to 2021, the team behind the paper built a model to understand the relationship between wildfire and climate. The researchers then repeatedly simulated worlds with and without climate change. This allowed them to isolate the impact of human-caused climate change versus normal, naturally occuring hot years, and to look at how various factors played a role. They found that human-caused warming was responsible for nearly all of...

This problem has been solved! You'll get a detailed solution from a subject matter expert that helps you learn core concepts. See Answer See Answer See Answer done loading Question:2. Explain the differences between western boundary currents, such as Gulf Stream, and eastern boundary currents, such as California Current, with respect to: (A) where they come from (low or high latitude); (B) the temperature of the water they transport (warm water/cold water); (C) their effect on coastal climate (do they make it warm and humid or cold and 2. Explain the differences between western boundary currents, such as Gulf Stream, and eastern boundary currents, such as California Current, with respect to: (A) where they come from (low or high latitude); (B) the temperature of the water they transport (warm water/cold water); (C) their effect on coastal climate (do they make it warm and humid or cold and dry?); (D) presence or absence of upwelling? (2 pts). 3. Describe the three factors factors that affect the intensity of wind-generated waves in the surface ocean? (1.5 pts) 4. List two erosional and two depositional landforms generated by wave action. (2 pts) Previous question Next question

The North Pacific Current (sometimes referred to as the North Pacific Drift) is an ocean current that flows west-to-east between Flows and temperature [ ] Originating from the eastward directed flow occurring east of the island of Honshu, Japan, the North Pacific Current extends over 40° of longitude. According to the Great Soviet Encyclopedia, the NPC may be considered to be a part or an extension of the Kuroshio current. The current covers a large area and brings warmer water from the subtropics to the sub-polar latitudes. Average sea surface temperature along the NPC can range in the winter from 45-61°F (7.2-16.1°C) and in the summer months 64°F-74°F (17.8-23.3°C). As it flows from west to east, the latitudinal extent of the NPC increases so much that it spans some 20 degrees of latitude east of the dateline. This is associated with a decrease in the speed of current; eastward directed speeds at the surface are typically less than 0.05 m/s (5 cm/s) in the central Pacific. As the NPC approaches the west coast of North America, it divides into two broad currents: the northward flowing Alaska Current and the southward flowing California Current. The splitting of flow is referred to as the The Gulf of Alaska and the California Current receive different volumes and flows of warm water from the North Pacific Current. The Gyre contribution [ ] The NPC forms the northward portion of the [ citation needed] References [ ]