Words That End In Iod 5 Letters

Words That End In Iod 5 Letters – Wordle has about thirteen thousand five-letter word predictions. It’s a great pool of words to choose from when you start, but your choices are narrow and things get more complicated as the game progresses. If you’ve got the second and third or third and fourth letters down, but you’re having trouble thinking of any words, don’t worry, we’re here to help. Check out some helpful Wordle tips below that are the middle ground of OD.

Our word list is taken from the Wordle dictionary, so all the tips here are valid guesses in Wordle. If you need more help, you can use our Wordle helper. Using our tool, you can get word suggestions by entering the current state of your game, including the letters you find in the correct and incorrect positions.

Words That End In Iod 5 Letters

Here’s a list of potential five-letter words you can use in Wordle, with OD in one of the two middle positions.

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When it comes to Wordle, not all words are created equal. From the tips above, there are techniques you can use to choose the best word. A general rule of thumb is to choose words with the most popular vowels and consonants. Also, it is best to avoid words with repeated letters. You can use our Wordle beginner’s guide to help you.

Hopefully this list of five letter words with OD in the middle has helped you with your Wordle game and you’ve figured out the word of the day. Check out Wordle’s other helpful tips for future daily puzzles. Impact of the Pacific Interdecadal Oscillation on Super Cyclone Activity in the Bay of Bengal During the Initial Cyclone Period

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Joint distribution analysis of forest fires and rainfall in response to ENSO, IOD and MJO (Case Study: Sumatra, Indonesia)

Causal Pathways Linking Different Flavours Of Enso With The Greater Horn Of Africa Short Rains

Received: 1 March 2022 / Revised: 25 March 2022 / Accepted: 26 March 2022 / Published: 28 March 2022

(This article belongs to a special issue on Extreme Hydrometeorological Events: Climate Warming or Natural Climate Change)

To assess the impact of El Niño Southern Oscillation (ENSO), Indian Ocean Dipole (IOD) and Madden Julian Oscillation (MJO) on the occurrence of land and wildfires in Sumatra, copula-based joint distribution analysis and quadrant analysis (for extreme events) are used in this study. carried out. In this study, drought (number of days without rain) and precipitation anomalies were used as climate indicators, and hotspots were used as drought and wildfire indicators. Using data from 2001 to 2020, this study shows that ENSO and IOD strongly influence Sumatra hotspots with monsoon-type rainfall. Although the effect is not linear, the probability of more hotspots increases significantly, especially when combined with a strong El Niño and a weak El Niño and a positive IOD. Furthermore, the results show that a moderate El Niño has similar effects to a weak El Niño on the affected region, and the combination of a weak El Niño with a positive IOD can lead to effects similar to those of a strong El Niño. At the same time, this study showed that the MJO affects the first dry season hotspots in Sumatran regions with equatorial type rainfall. Although its impact on the dryland precipitation anomaly is unclear, phases 6, 7, and 8 of the MJO significantly increase the dependence on dry spells under dry conditions.

Land and forest fires; ENSO; IOD; MJO; copula; extreme analysis; Land and forest fires in Sumatra; ENSO; IOD; MJO; copula; extreme analysis; Sumatra

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With the increase in global average temperature (global warming), some researchers point out that extreme climate change and occurrence has increased in recent decades [1, 2, 3]. If this trend continues, more serious fires may occur in the future [4]. Land and forest fires are an annual occurrence on the island of Sumatra. Due to the limited amount of historical data, it is necessary to analyze the multivariate distribution of forest and climate indicators to assist the government in predicting land and forest fires in Sumatra under the influence of future climate extremes. A 2013 study by [5] showed that land and forest fires in Sumatra are divided into two types according to the seasonal rainfall pattern in each region. Rainfall patterns are monsoonal and equatorial [6]. The monsoon rain pattern is a 12-month rain pattern, with the dry season occurring between June and August. Meanwhile, the equatorial rain pattern is a rain pattern with two dry season peaks within a year, namely around March and October, so it has a six-month long rainy season. The land and forest fire pattern associated with the monsoon pattern occurs in and around the South Sumatra region, while the equatorial pattern of land and forest fires occurs in and around the Riau region [5]. The characteristics of land and forest fires are reflected in the general scheme of forest and land fire indicators and precipitation in the region [7, 8].

A study [7] explains the relationship between burned area, carbon emissions and precipitation indicators using principal component analysis. The study found that area burned is more closely related to precipitation than to carbon emissions as a climate indicator. Monsoon forest and terrestrial fire patterns last 12 months, while equatorial forest fires last 6 months [7]. However, the contribution of equatorial forest and terrestrial fire patterns to the total data (annual signal) is very small compared to the monsoon. If the pre-processing data is not done properly (without separating the analyzed area without equatorial signal), the equatorial fire pattern may not be detected [8].

In addition to the influence of these two types of rainfall, rainfall variability (extreme/low rainfall) in Sumatra is influenced by global climate phenomena, namely the El Niño Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) [9]. ENSO is an anomalous event of above normal average sea surface temperatures in the Pacific Ocean off the west coast of Ecuador and Peru. ENSO consists of two phases, namely La Niña and El Niño [10]. The effect of El Niño on Indonesia is a delay in the rainy season and a decrease in the intensity of rainfall in Indonesia [9], which leads to a more severe dry season. At the same time, the IOD is a phenomenon of sea surface temperature oscillation in the western Indian Ocean, which is warmer (in positive phase) and cooler (in negative phase) than in the eastern Indian Ocean on a non-uniform basis [11] . A biphasic positive IOD phenomenon can reduce precipitation around the western IOD SST (from 50° E to 70° E and from 10° to 10° N) and increase the severity of the dry season in the southern part of the country. When Sumatra emerged during the dry season [9]. Therefore, when El Niño and a positive IOD occur at the same time, the strengthening of the dry season in southern Sumatra will be more significant.

A study by [12] in 2021 showed that El Niño and positive IOD were also positively correlated with land and forest fires in Sumatra. This is confirmed by the increase in scale and duration of forest and land fire events that occur in association with El Niño and/or positive IOD [ 13 ]. The study [13] also explains that the increase in the scale of the occurrence of land and forest fire phenomenon is not linear with the strengthening of El Niño and/or IOD, and not all land and forest fires in Sumatra are affected.

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