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was ist was stream

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Please send me updates about products and services of Ververica via my e-mail address. What is stream processing? Actions and analytics are up-to-date, reflecting the data when it is still fresh, meaningful, and valuable.

Stream processing can handle data volumes that are much larger than other data processing systems: The event streams are processed directly, and only a meaningful subset from the data is persisted.

Incrementally computing updates, rather than periodic recomputation of all data fits naturally with the stream processing model. Stream processing decentralizes and decouples the infrastructure: The streaming paradigm reduces the need for large and expensive shared databases.

Instead, each stream processing application maintains its own data and state, which is made simple by the stream processing framework.

In this way, a stream processing application fits naturally in a microservices architecture. Each new transaction is compared to those in the state, labeled as valid or fraudulent, and the state is updated with that transaction.

Each product interaction generates an event that updates these parameters. When Adolf Hitler reawakens at the site of his former bunker 70 years later, he's mistaken for a brilliant comedian and becomes a media phenomenon.

Watch all you want for free. More Details. Watch offline. Available to download. Microsoft Stream also helps you organize content into channels and groups so it's easier to find.

Microsoft Stream works well with other Office apps like Teams, SharePoint, OneNote, and Yammer, giving even more ways to discover more relevant content.

Get started with Microsoft Stream in minutes and view videos on all your devices from anywhere, anytime.

For more details about a particular topic, see the table of contents. Skip to main content.

Was Ist Was Stream - Was ist Was TV auf DVD und Blu-ray

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A stream is a body of water [1] with surface water flowing within the bed and banks of a channel. The flow of a stream is controlled by three inputs - surface water, subsurface water and groundwater.

The surface and subsurface water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation.

Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers.

Streams are important as conduits in the water cycle , instruments in groundwater recharge , and corridors for fish and wildlife migration.

The biological habitat in the immediate vicinity of a stream is called a riparian zone. Given the status of the ongoing Holocene extinction , streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity.

The study of streams and waterways in general is known as surface hydrology and is a core element of environmental geography.

Streams typically derive most of their water from precipitation in the form of rain and snow.

Most of this water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants.

Some of the water proceeds to sink into the earth by infiltration and becomes groundwater , much of which eventually enters streams.

Some precipitated water is temporarily locked up in snow fields and glaciers , to be released later by evaporation or melting. The rest of the water flows off the land as runoff , the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief.

This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth.

Some creeks may start from ponds or lakes. To qualify as a stream, a body of water must be either recurring or perennial. Recurring intermittent streams have water in the channel for at least part of the year.

A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it.

When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream.

Streams of lower order joining a higher order stream do not change the order of the higher stream. Thus, if a first-order stream joins a second-order stream, it remains a second-order stream.

It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream.

The gradient of a stream is a critical factor in determining its character and is entirely determined by its base level of erosion.

The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream.

In geological terms, the stream will erode down through its bed to achieve the base level of erosion throughout its course.

If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander.

Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials.

These are typically serpentine in form. Typically, over time the meanders gradually migrate downstream.

If some resistant material slows or stops the downstream movement of a meander, a stream may erode through the neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou.

A flood may also cause a meander to be cut through in this way. Typically, streams are said to have a particular profile , beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders.

The initial stage is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream.

This simplifies the overall infrastructure, because many systems can be built on a common architecture, and also allows a developer to build applications that use analytical results to respond to insights in the data—to take action—directly.

Interested in learning more? Privacy Policy. Please send me updates about products and services of Ververica via my e-mail address.

What is stream processing? Actions and analytics are up-to-date, reflecting the data when it is still fresh, meaningful, and valuable.

Stream processing can handle data volumes that are much larger than other data processing systems: The event streams are processed directly, and only a meaningful subset from the data is persisted.

Incrementally computing updates, rather than periodic recomputation of all data fits naturally with the stream processing model. Stream processing decentralizes and decouples the infrastructure: The streaming paradigm reduces the need for large and expensive shared databases.

Instead, each stream processing application maintains its own data and state, which is made simple by the stream processing framework.

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